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1

ARM - PI Product - SGP and TWP (Manus) Ice Cloud Vertical Velocities  

NLE Websites -- All DOE Office Websites (Extended Search)

ProductsSGP and TWP (Manus) Ice Cloud Vertical ProductsSGP and TWP (Manus) Ice Cloud Vertical Velocities Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send PI Product : SGP and TWP (Manus) Ice Cloud Vertical Velocities 1997.01.01 - 2010.12.31 Site(s) SGP TWP General Description Daily netcdf-files of ice-cloud dynamics observed at the ARM sites at SGP (Jan1997-Dec2010) and Manus (Jul1999-Dec2010). The files include variables at different time resolution (10s, 20min, 1hr). Profiles of radar reflectivity factor (dbz), Doppler velocity (vel) as well as retrieved vertical air motion (V_air) and reflectivity-weighted particle terminal fall velocity (V_ter) are given at 10s, 20min and 1hr resolution. Lower level clouds are removed, however a multi-layer flag is included.

2

Characterization of Surface Albedo Over the ARM SGP CART and the NSA  

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Characterization of Surface Albedo Characterization of Surface Albedo Over the ARM SGP CART and the NSA Z. Li and M. C. Cribb Earth System Science Interdisciplinary Center University of Maryland College Park, Maryland A. P. Trishchenko and Y. Luo Canada Centre for Remote Sensing Ottawa, Ontario, Canada Introduction Surface albedo is needed for satellite remote sensing of the surface radiation budget and for climate modelling. Determination of areal-mean surface albedo is challenging. Over the Southern Great Plains (SGP) site, a primary challenge lies in the inhomogeneity associated with different land cover types. Over the North Slope of Alaska (NSA) site, persistent cloud cover renders remote sensing of surface albedo difficult. We tackle both challenges following two different approaches. Over the SGP site, we

3

ARM - TWP Science  

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PacificTWP Science PacificTWP Science TWP Related Links Facilities and Instruments Manus Island Nauru Island Darwin, AUS ES&H Guidance Statement Operations Science Field Campaigns Year of Tropical Convection Visiting the Site TWP Fact Sheet Images Information for Guest Scientists Contacts TWP Science New VSAT dish installed in the Tropical Western Pacific. New VSAT dish installed in the Tropical Western Pacific. The following are the basic science goals of the TWP component of the ARM Climate Research Facility: Determine the magnitude of the surface radiation budget terms and determine their spatial and temporal variability. Identify bulk and optical properties of clouds in the TWP and how these properties affect the radiation budget. Understand the linkages among sea surface temperature,

4

ARM - Visiting the TWP  

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PacificVisiting the TWP PacificVisiting the TWP TWP Related Links Facilities and Instruments Manus Island Nauru Island Darwin, AUS ES&H Guidance Statement Operations Science Field Campaigns Year of Tropical Convection Visiting the Site TWP Fact Sheet Images Information for Guest Scientists Contacts Visiting the TWP Nauru Island from the air. Nauru Island from the air. The Tropical Western Pacific site consists of three diverse climate research facilities in Papua New Guinea, the Republic of Nauru, and Australia. Each facility has its own operating procedures and health and safety issues. Safety First! Before visiting any of the three TWP facilities, you must do the following: Submit a Site and Computer Access Request Form Read the Safety Plan for the facility you plan to visit: TWP Site Visit Safety Procedure

5

TWP Darwin Site  

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Darwin Site Darwin Site TWP Related Links Facilities and Instruments Manus Island Nauru Island Darwin, AUS ES&H Guidance Statement Operations Science Field Campaigns Year of Tropical Convection Visiting the Site TWP Fact Sheet Images Information for Guest Scientists Contacts TWP Darwin Site Location: 12° 25' 28.56" S, 130° 53' 29.75" E Altitude: 29.9 meters The third TWP climate research facility was established in April 2002 in Darwin, Northern Territory, Australia. The facility is situated adjacent to the Australian Bureau of Meteorology's (BOM) Meteorological Office near Darwin International Airport. Darwin was chosen because it meets the scientific goal of the ARM Program, providing a unique set of climate regimes that are not seen at the other TWP facilities. Annually, Darwin

6

TWP Nauru Site  

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Nauru Site Nauru Site TWP Related Links Facilities and Instruments Manus Island Nauru Island Darwin, AUS ES&H Guidance Statement Operations Science Field Campaigns Year of Tropical Convection Visiting the Site TWP Fact Sheet Images Information for Guest Scientists Contacts TWP Nauru Site Location: 0° 31' 15.6" S, 166° 54' 57.60" E Altitude: 7.1 meters The Nauru facility was established in November 1998 as the second TWP climate research station. It is situated in the Denigomodu district on Nauru Island, the Republic of Nauru, which is located in the western South Pacific, approximately 1,200 miles northeast of Papua New Guinea. The ARM Program selected this location because it is on the eastern edge of the Pacific warm pool under La Niña conditions, which affect weather patterns

7

ARM - TWP Nauru Site  

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Nauru Site Nauru Site TWP Related Links Facilities and Instruments Manus Island Nauru Island Darwin, AUS ES&H Guidance Statement Operations Science Field Campaigns Year of Tropical Convection Visiting the Site TWP Fact Sheet Images Information for Guest Scientists Contacts TWP Nauru Site Location: 0° 31' 15.6" S, 166° 54' 57.60" E Altitude: 7.1 meters The Nauru facility was established in November 1998 as the second TWP climate research station. It is situated in the Denigomodu district on Nauru Island, the Republic of Nauru, which is located in the western South Pacific, approximately 1,200 miles northeast of Papua New Guinea. The ARM Program selected this location because it is on the eastern edge of the Pacific warm pool under La Niña conditions, which affect weather patterns

8

ARM - TWP Contacts  

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Contacts Contacts TWP Related Links Facilities and Instruments Manus Island Nauru Island Darwin, AUS ES&H Guidance Statement Operations Science Field Campaigns Year of Tropical Convection Visiting the Site TWP Fact Sheet Images Information for Guest Scientists Contacts TWP Contacts Site Oversight - Kim Nitschke, Los Alamos National Laboratory Site Manager - Paul Ortega, Los Alamos National Laboratory Site Operations Manager - Matt Gould, Australian Bureau of Meteorology Site Scientist - Chuck Long, Pacific Northwest National Laboratory Tropical Western Pacific Office Mailing Address: Los Alamos National Laboratory PO Box 1663, MS J577 Los Alamos, NM 87545 U.S.A. Shipping Address: SM-30 Bikini Atoll Road TA-51, Bldg. 82, DP 01U Attn: NAME, MS J577 Los Alamos, NM 87545 U.S.A. Phone: 505.667.1186

9

ARM - Visiting the SGP  

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PlainsVisiting the SGP PlainsVisiting the SGP SGP Related Links Facilities and Instruments Central Facility Boundary Facility Extended Facility Intermediate Facility Radiometric Calibration Facility Geographic Information ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Fact Sheet Images Information for Guest Scientists Contacts Visiting the SGP View a custom Google map with driving directions to the SGP Central Facility. View a custom Google map with driving directions to the SGP Central Facility. Safety First! Before visiting the SGP, you must submit a Site Access Request Form. When visiting the site, you must attend a safety orientation given by the Site Operations Manager. Environmental Safety and Health Documents The Environmental Safety and Health (ES&H) documents listed below are

10

ARM - NSA Operations  

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Images Information for Guest Scientists Contacts NSA Operations Barrow Facility Instrumentation at the Barrow facility operates 7 days a week, 24 hours a day, year around. The...

11

ARM - NSA Calendar  

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the Site Images Information for Guest Scientists Contacts NSA Calendar Alan JensenTower Systems Tower inspection, maintenance and installation of lighting kit 2013.10.02 ...

12

NSA-Beaver Pond Site  

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Beaver Pond Site (NSA-BP) Beaver Pond Site (NSA-BP) The storage tent and gas collectors NSA-BP site looking to the east. Visible is the investigator hut on drier land to the west and the boardwalk leading out to the tower site in the right portion of the image with the mounded beaver lodge visible in the middle of the image. The bridge and the 3 meter flux tower The beaver lodge The bridge from the flux tower This is the floating bridge leading from the flux tower back to the shore. The large tent for holding equipment is clearly visible on the shore. The TGB gas collectors on the beaver pond Back to the BOREAS Photo Page Index Other Sites: NSA Photos ||NSA-BP Photos | NSA-Fen Photos | NSA-OA Photos | NSA-OBS Photos | NSA-OJP Photos | NSA-UBS Photos | NSA-YJP Photos | NSA-Ops Photos

13

ARM - NSA Science  

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AlaskaNSA Science AlaskaNSA Science NSA Related Links Facilities and Instruments Barrow Atqasuk ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Images Information for Guest Scientists Contacts NSA Science Scientific objectives for the NSA/AAO site are provided below: Provide the comprehensive data sets necessary to develop and test continually improved algorithms for GCMs to describe radiative transfer and cloud processes at high latitudes; Specifically focus on development of algorithms to describe: radiative transfer within both the clear and cloudy atmosphere, especially at low temperatures; physical and optical behavior of water (ice) and land surfaces, both bare and snow-covered, especially during transitions from winter to summer and back; physical and optical behavior of ice and mixed phase clouds.

14

ARM - SGP Operations  

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Operations Operations SGP Related Links Facilities and Instruments Central Facility Boundary Facility Extended Facility Intermediate Facility Radiometric Calibration Facility Geographic Information ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Fact Sheet Images Information for Guest Scientists Contacts SGP Operations Routine Operations SGP central facility offices. SGP central facility offices. The overwhelming majority of the measurements with the highest priority, on which the existing experimental designs are based, are regular routine observations, as specified in the ARM Program Plan, 1990 (U.S. Department of Energy 1990). Scientifically and logistically, routine operations also serve as the basis and background for all nonroutine operations, including

15

Slide 1  

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reflectivities, vertical velocities, and Doppler spectral widths * "Old" ARSCL - Availability via ARM archive SGP - 111996 thru 92007 NSA - 31998 thru 92007 TWP-C1 - 799 -...

16

Orr 2007 ARM STM poster2.ppt  

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Responsible for management and maintenance of nearly all data and instrument computers as well as personal computers at the ACRF sites (AMF, NSA, SGP and TWP). Cyber...

17

ARM - Visiting the NSA  

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Site Images Information for Guest Scientists Contacts Visiting the NSA View a custom Google map with driving directions to the Barrow site. Zoom in on the map for more detail....

18

ARM - SGP Science  

NLE Websites -- All DOE Office Websites (Extended Search)

Science Science SGP Related Links Facilities and Instruments Central Facility Boundary Facility Extended Facility Intermediate Facility Radiometric Calibration Facility Geographic Information ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Fact Sheet Images Information for Guest Scientists Contacts SGP Science Overall Objectives The primary goal of the Southern Great Plains (SGP) site is to produce data adequate to support significant research addressing the objectives of the overall ARM Climate Research Facility. These overall objectives, as paraphrased from the ARM Program Plan (DOE 1990), are the following: to describe the radiative energy flux profile of the clear and cloudy atmosphere to understand the processes determining the flux profile

19

NSA-Fen Site  

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NSA-Fen) NSA-Fen) The Fen from the air, looking North. You can see the boardwalk, the hut, and the size of the bog. The road (Highway 391) is visible at the top. The round "crater" near the base of the boardwalk on the right is a collapsed palsa. View an aerial photo-map of the NSA-Fen site. The ground cover on the Fen itself The hut and flux tower The Fen site from the shore looking toward the hut The Fen site flux tower The boardwalk in the Fen, looking back at the shore The generator shed and the storage tent The NSA-Fen site from the air during IFC-2. Top of image is to Southeast. The NSA-Fen site in September (IFC-3) 1994 looking to the southeast. The tower is at the end of the boardwalk in right center of image with the hut near the center. The boardwalk connects to the far border at left center of the slide. Note that the tamarack (deciduous evergreen) within the fen has its fall colors.

20

SGP Central Facility  

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Central Facility Central Facility SGP Related Links Facilities and Instruments Central Facility Boundary Facility Extended Facility Intermediate Facility Radiometric Calibration Facility Geographic Information ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Fact Sheet Images Information for Guest Scientists Contacts SGP Central Facility The ARM Climate Research Facility deploys specialized remote sensing instruments in a fixed location at the site to gather atmospheric data of unprecedented quality, consistency, and completeness. More than 30 instrument clusters have been placed around the site; the central facility; and the boundary, intermediate, and extended facilities. The locations for the instruments were chosen so that the measurements reflect conditions

Note: This page contains sample records for the topic "nsa sgp twp" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


21

ARM - SGP Central Facility  

NLE Websites -- All DOE Office Websites (Extended Search)

Central Facility Central Facility SGP Related Links Facilities and Instruments Central Facility Boundary Facility Extended Facility Intermediate Facility Radiometric Calibration Facility Geographic Information ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Fact Sheet Images Information for Guest Scientists Contacts SGP Central Facility The ARM Climate Research Facility deploys specialized remote sensing instruments in a fixed location at the site to gather atmospheric data of unprecedented quality, consistency, and completeness. More than 30 instrument clusters have been placed around the site; the central facility; and the boundary, intermediate, and extended facilities. The locations for the instruments were chosen so that the measurements reflect conditions

22

NSA Barrow Facility  

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Barrow Facility Barrow Facility NSA Related Links Facilities and Instruments Barrow Atqasuk ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Images Information for Guest Scientists Contacts NSA Barrow Facility Location: 71° 19' 23.73" N, 156° 36' 56.70" W Altitude: 8 meters The Barrow facility was dedicated in July 1997 and chosen because the Arctic is particularly sensitive to climate changes. Barrow is located at the northernmost point in the United States, 330 miles north of the Arctic Circle. Also known as the Top of the World, Barrow is Alaska's largest Eskimo village (home to 4,581 people). Tax revenue from the Slope's oil fields pay for services borough wide, and natural gas is used to heat homes and generate electricity in Barrow. Many residents, however, maintain

23

ARM - NSA Barrow Facility  

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Barrow Facility Barrow Facility NSA Related Links Facilities and Instruments Barrow Atqasuk ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Images Information for Guest Scientists Contacts NSA Barrow Facility Location: 71° 19' 23.73" N, 156° 36' 56.70" W Altitude: 8 meters The Barrow facility was dedicated in July 1997 and chosen because the Arctic is particularly sensitive to climate changes. Barrow is located at the northernmost point in the United States, 330 miles north of the Arctic Circle. Also known as the Top of the World, Barrow is Alaska's largest Eskimo village (home to 4,581 people). Tax revenue from the Slope's oil fields pay for services borough wide, and natural gas is used to heat homes and generate electricity in Barrow. Many residents, however, maintain

24

TWP Island Cloud Trail Studies  

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Pacific Island Cloud Trail Studies Pacific Island Cloud Trail Studies W. M. Porch Los Alamos National Laboratory Los Alamos, New Mexico S. Winiecki University of Chicago Chicago, Illinois Introduction Images and surface temperature measurements from the U.S. Department of Energy (DOE) Multi- spectral Thermal Imaging (MTI) satellite are combined with geostationary meteorological satellite (GMS) images during 2000 and 2001 to better understand cloud trail formation characteristics from the Atmospheric Radiation Measurement (ARM) Tropical Western Pacific (TWP) site. Figure 1 shows a comparison on two consecutive days in December 2000. The day for which a cloud trail developed was more moist and cooler at the altitude the cloud developed (about 600 m) and there was very little

25

Surface Meteorological Instruments for TWP (SMET) Handbook  

Science Conference Proceedings (OSTI)

The TWP Surface Meteorology station (SMET) uses mainly conventional in situ sensors to obtain 1-minute statistics of surface wind speed, wind direction, air temperature, relative humidity, barometric pressure and rainfall amount.

Ritsche, MT

2009-01-01T23:59:59.000Z

26

SGP Shipment Notification Form  

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PlainsShipment Notification Form PlainsShipment Notification Form SGP Related Links Facilities and Instruments Central Facility Boundary Facility Extended Facility Intermediate Facility Radiometric Calibration Facility Geographic Information ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Fact Sheet Images Information for Guest Scientists Contacts Shipment Notification Form Note: Red text indicates a required field. Your Notification Form has been submitted. Section 1 : Initiator Information Date Afilliation Name Phone Number Email Section 2 : Vendor Information Ship From Point of Contact Address Phone Section 3 : Carrier Information Shipping Company Tracking/AWB Number Number of Boxes Approximate Weight for EACH BOX Expected Ship Date Section 4 : Shipment List Description System/Instrument

27

NSA-Old Jack Pine Site  

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NSA-OJP) Aerial view of the NSA-OJP site during IFC 2. The Rohn tower and investigator hut are in the approximate center of the image with the generator hut at the extreme upper...

28

A TWP-ICE High-Level Cloud Case Study  

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A TWP-ICE High-Level Cloud Case Study Mace, Gerald University of Utah Category: Field Campaigns The Tropical Warm Pool International Cloud Experiment (TWP ICE) was conducted near...

29

Heating Profiles Derived From Cm-wavelength Radar During TWP...  

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Heating Profiles Derived From Cm-wavelength Radar During TWP-ICE Heating Profiles Derived From Cm-wavelength Radar During TWP-ICE Courtney Schumacher and Kaycee Frederick Courtney...

30

ARM - SGP Rural Driving Hazards  

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Rural Driving Hazards Rural Driving Hazards SGP Related Links Facilities and Instruments Central Facility Boundary Facility Extended Facility Intermediate Facility Radiometric Calibration Facility Geographic Information ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Fact Sheet Images Information for Guest Scientists Contacts SGP Rural Driving Hazards The rural location of the Southern Great Plains (SGP) site facilities requires that visitors travel on unpaved, dirt and gravel, roads. Visitors should be aware of the driving hazards this presents by taking the following precautions: Proceed cautiously: Many rural roads have unmarked and blind intersections. Slow down: Sanded and gravel raods can cause a vehicle to swerve. Maintain a safe following distance: During the dry season, vehicles

31

ARM - Publications: Science Team Meeting Documents  

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The ARM-UAV Grand Tour, SGP, NSA, TWP Tooman, T.T., Bolton, W.B.(a), and McCoy, R.F.(a), Sandia National Laboratories (a) Thirteenth Atmospheric Radiation Measurement (ARM) Science...

32

AVESTAR® - Shale Gas Processing (SGP)  

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Shale Gas Processing (SGP) Shale Gas Processing (SGP) SPG The shale gas revolution is transforming America's energy landscape and economy. The shale gas boom, including the Marcellus play in Appalachia, is driving job creation and investment in the energy sector and is also helping to revive other struggling sectors of the economy like manufacturing. Continued growth in domestic shale gas processing requires that energy companies maximize the efficiency and profitability from their operations through excellent control and drive maximum business value from all their plant assets, all while reducing negative environmental impact and improving safety. Changing demographics and rapidly evolving plant automation and control technologies also necessitate training and empowering the next-generation of shale gas process engineering and

33

NSA-Old Black Spruce Site  

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NSA-OBS) NSA-OBS) The NSA-OBS site from the air. This aerial shot of the OBS site shows the generator in the lower-right corner, one of the huts in the upper-left corner, and part of the boardwalk leading away from the hut. View an aerial photo-map of the NSA-OBS site. OBS spruce trees and flux tower The road to the OBS site. The road to the OBS site was often a muddy mess, accessable only by ARGO all-terrain vehicles, and even they got stuck often. The OBS flux tower The NSA black spruce carbon model evaluation site and TE canopy access tower. Oblique view of the trail leading into the NSA Old Black Spruce site. Highway 391 is beyond the image at the bottom and the power line is viewable at the top of the image. The NSA-OBS site would be off to the upper left. The NSA-OBS Rohn tower where Amar Bazzaz of Harvard University is climbing the tower for maintenance.

34

ARM - Field Campaign - SGP99 IOP  

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govCampaignsSGP99 IOP govCampaignsSGP99 IOP Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Campaign : SGP99 IOP 1999.07.07 - 1999.07.22 Lead Scientist : Richard Cederwall Summary The Southern Great Plains 1997 Hydrology Experiment (SGP97) successfully demonstrated the ability to map and monitor soil moisture using low frequency microwave radiometers (L band, 1.4 GHz). Soil moisture retrieval algorithms developed using higher resolution data were proven to be extendible to coarser resolution (Jackson et al., 1999). Figure 1 shows one sequence of soil moisture observations obtained in SGP97. The resulting data set will be the focus of a wide variety of value added scientific research in hydrology, meteorology, and climate. SGP97 also developed a

35

Progress on a TWP-ICE Monsoon Case Study  

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25-mb 25-mb large-scale forcing 10-mb large-scale forcing Tracers Future work Progress on a TWP-ICE Monsoon Case Study Ann Fridlind and Andrew Ackerman * NASA GISS thanks to Jon Petch * ECMWF Shaocheng Xie * LLNL TWP-ICE and ACTIVE Science Teams DOE ARM Program and Data Archive NASA Radiation Sciences Program NASA Advanced Supercomputing Division 18th Annual ARM Science Team Meeting 10 March 2008 Outline Introduction 25-mb large-scale forcing 10-mb large-scale forcing Tracers Future work 1 Introduction TWP-ICE monsoon period GISS set-up 2 25-mb large-scale forcing Initial results Comparison with ECMWF forcing style Tropopause moisture analysis 3 10-mb large-scale forcing Tropopause moisture analysis Final results 4 Tracers Measurements Model results 5 Future work Outline Introduction 25-mb large-scale forcing 10-mb large-scale forcing Tracers Future work TWP-ICE monsoon

36

The TWP-ICE CRM Intercomparison Specification and First Results  

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TWP-ICE CRM Intercomparison Specification and First Results Ann Fridlind (ann.fridlind@nasa.gov), Andrew Ackerman (andrew.ackerman@nasa.gov), Adrian Hill (adrian.hill@metoffice.gov...

37

Interpolation Uncertainties Across the ARM SGP Area  

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Interpolation Uncertainties Across the ARM SGP Area Interpolation Uncertainties Across the ARM SGP Area J. E. Christy, C. N. Long, and T. R. Shippert Pacific Northwest National Laboratory Richland, Washington Interpolation Grids Across the SGP Network Area The U.S. Department of Energy (DOE) Atmospheric Radiation Measurement (ARM) Program operates a network of surface radiation measurement sites across north central Oklahoma and south central Kansas. This Southern Great Plains (SGP) network consists of 21 sites unevenly spaced from 95.5 to 99.5 degrees west longitude, and from 34.5 to 38.5 degrees north latitude. We use the technique outlined by Long and Ackerman (2000) and Long et al. (1999) to infer continuous estimates of clear-sky downwelling shortwave (SW) irradiance, SW cloud effect, and daylight fractional sky cover for each

38

ARM/NSA Vehicle Use Policy  

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Operating Procedures for Scaffold Use October 2007 Operating Procedures for Scaffold Use October 2007 Atmospheric Radiation Measurement Climate Research Facility/ North Slope of Alaska/Adjacent Arctic Ocean (ACRF/NSA/AAO) Operating Procedures for The Use of Scaffolds at ACRF/NSA/AAO Meteorological Towers Introduction: An aluminum scaffold structure is used at ARM Climate Research Facility/North Slope of Alaska/Adjacent Arctic Ocean (ACRF/NSA/AAO) Sites to access instruments mounted on the meteorological tower as shown in Figure 1 below. The scaffold is typically used for maintenance of instruments mounted on moveable booms or for maintenance of guest or temporary instruments. The scaffold is a commercially-available product that was purchased from Upright, Inc. and was fitted with aluminum grating platforms by Cubic Designs, Inc. of

39

ARM - PI Product - NSA AERI Hatch Correction Data Set  

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ProductsNSA AERI Hatch Correction Data Set Comments? We would love to hear from you Send us a note below or call us at 1-888-ARM-DATA. Send PI Product : NSA AERI Hatch Correction...

40

Darwin: The Third DOE ARM TWP ARCS Site  

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Darwin: The Third DOE ARM TWP ARCS Site Darwin: The Third DOE ARM TWP ARCS Site W. E. Clements and L. Jones Los Alamos National Laboratory, Los Alamos, New Mexico T. Baldwin Special Services Unit Australian Bureau of Meteorology Melbourne, Australia K. Nitschke South Pacific Regional Environment Programme Apia, Samoa Introduction The U.S. Department of Energy's (DOE's) Atmospheric Radiation Measurement (ARM) Program began operations in its Tropical Western Pacific (TWP) locale in October 1996 when the first Atmospheric Radiation and Cloud Station (ARCS) began collecting data on Manus Island in Papua New Guinea (PNG). Two years later, in November 1998 a second ARCS began operations on the island of Nauru in the Central Pacific. Now a third ARCS has begun collecting data in Darwin, Australia. See Figure 1 for

Note: This page contains sample records for the topic "nsa sgp twp" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


41

Title: Radar-observed convective characteristics during TWP-ICE  

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Title: Radar-observed convective characteristics during TWP-ICE Title: Radar-observed convective characteristics during TWP-ICE Schumacher, Courtney Texas A&M University Houze, Robert University of Washington May, Peter Bureau or Meteorology Research Centre Frederick, Kaycee Cetrone, Jasmine Vallgren, Andreas Category: Field Campaigns This poster will describe the radar dataset obtained in the Tropical Warm Pool International Cloud Experiment (TWP-ICE), which is to take place 20 January - 14 February 2006 in the vicinity of Darwin, Australia. We will describe the convective systems observed during the project by two scanning C-band Doppler radars, one of which will provide dual-polarization measurements, and ARM's vertically pointing cloud radar and lidar installations. In addition, we will discuss the potential for combining

42

TWP93.0100104 DOC#: TWP-DOC-1.4 SCIENCE AND SITING STRATEGY FOR THE  

NLE Websites -- All DOE Office Websites (Extended Search)

TWP93.0100104 TWP93.0100104 DOC#: TWP-DOC-1.4 SCIENCE AND SITING STRATEGY FOR THE TROPICAL WESTERN PACIFIC ARM CART LOCALE Thomas P. Ackerman The Pennsylvania State University Bill Clements Fairley Barnes Los Alamos National Laboratory David S. Renné National Renewable Energy laboratory Science and Siting Strategy for the Tropical Western Pacific ARM CART Locale Ackennan, T., B. Clements, F. Barnes, and D. Renne DISCLAIMER This is a working document of the Tropical Western Pacific Program of the United States Department of Energy's Atmospheric Radiation Measurement Program. It is updated periodically and this release may not reflect the most current status of the program. It should not be quoted without consultation with the authors and specific reference to this disclaimer.

43

ARM - NSA Atqasuk Facility-Inactive  

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Atqasuk Facility-Inactive Atqasuk Facility-Inactive NSA Related Links Facilities and Instruments Barrow Atqasuk ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Images Information for Guest Scientists Contacts NSA Atqasuk Facility-Inactive Location: 70° 28' 19.11" N, 157° 24' 28.99" W Altitude: 20 meters The Atqasuk facility, which was part of the larger ARM Climate Research Facility (ARM) North Slope of Alaska site, was installed the summer of 1999 off of a road near the Atqasuk Airport and operated through 2010. Located approximately 70 miles south of Barrow, Atqasuk is adjacent to the Meade River. Its climate is much more continental than that of Barrow. Atqasuk (population 225) has an economy that is largely based on subsistence fishing and caribou hunting. The Atqasuk community

44

Investigation of Unusual Albedos in the SGP Domain  

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Investigation of Unusual Albedos in the SGP Domain Investigation of Unusual Albedos in the SGP Domain Groff, David ARM SGP Duchon, Claude University Of Oklahoma Category: Atmospheric State and Surface We investigate the cause of unusually high albedos at an Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) extended facility near Morris, OK. In a previous study, daily albedos were calculated at several SGP extended facilities for 1998 and 1999 using broadband (.28 to 3 microns) pyranometers. The average daily albedo during this period was calculated to be at least about 5% higher at Morris than at any of the other SGP extended facilities. Surface based measurements of daily albedos at Morris and two nearby SGP extended facilities during 2004 and 2005 suggest the unusually high albedo measurements at Morris are real.

45

ARM - SGP Geographic Information By Facility  

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Geographic Information By Facility Geographic Information By Facility SGP Related Links Facilities and Instruments Central Facility Boundary Facility Extended Facility Intermediate Facility Radiometric Calibration Facility Geographic Information ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Fact Sheet Images Information for Guest Scientists Contacts SGP Geographic Information By Facility Note: BF = Boundary Facility, EF = Extended Facility, and IF = Intermediate Facility Site Elevation (m) Lat./Long. Surface Type Anthony, Kansas: EF31 412 37.151 N -98.362W Pasture Ashton, Kansas: EF9 386 37.133 N 97.266 W Pasture Beaumont, Kansas: IF1 (Removed 4/12/2011) 478 37.626 N 96.538 W Rangeland Billings, OK (XSAPR Radar): IF4 330 36.579 N 97.364 W Cultivated Field Billings, OK (915 MHz RWP): IF9 291 36.476 N

46

ARM/NSA Vehicle Use Policy  

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6 6 Tip Tower Lowering Procedure November 2006 Atmospheric Radiation Measurement Climate Research Facility/ North Slope of Alaska/Adjacent Arctic Ocean NSA Tip Tower Lowering Procedure Procedure Summary: The tip tower is hinged approximately 6 feet above the ground. A set of weights permanently positioned on the lower portion of the tower are used to counterbalance the weight of the tower as it is lowered. To assist in tower lowering, a nylon line, fastened to the mid-section of the tower, is used to pull the tower downward. In the lowered position, a hinged wood frame supports the top of the tower while instrument maintenance is performed. Following instrument maintenance, the counterweights are used to naturally pull the tower back to an upright position

47

New Surface Meteorological Measurements at SGP,  

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NM, March 22 - 26, 2004 NM, March 22 - 26, 2004 1 New Surface Meteorological Measurements at SGP, and Their Use for Assessing Radiosonde Measurement Accuracy L.M. Miloshevich National Center for Atmospheric Research Boulder, Colorado B.M. Lesht and M. Ritche Argonne National Laboratory Argonne, Illinois Introduction Several recent ARM investigations have been directed toward characterizing and improving the accuracy of ARM radiosonde water vapor measurements. Tobin et al. (2002) showed that calculating the downwelling and outgoing longwave fluxes with a target accuracy of 1 W m -2 requires knowing the total-column precipitable water vapor (PW) with 2% absolute accuracy and knowing the upper troposphere (UT) water vapor with 10% absolute accuracy. Turner et al. (2003) used an empirical

48

Microsoft Word - SGP CART Safety Orientation.doc  

NLE Websites -- All DOE Office Websites (Extended Search)

4-002 4-002 SGP CART SAFETY ORIENTATION Page 1 of 1 SGP CART SAFETY ORIENTATION Revised 10/14/04 1 INTRODUCTION Welcome to the Atmospheric Radiation Measurement Program's Southern Great Plains (SGP) Climate Research Facility. Argonne National Laboratory (ANL) manages this U.S. Department of Energy (DOE) site. It is very important that all visitors comply with all DOE and ANL safety requirements, as well as those of the Occupational Safety and Health Administration (OSHA), the National Fire Protection Association, and the U.S. Environmental Protection Agency, and with other requirements as applicable. 2 VISITOR SIGN-IN AND SIGN-OUT All visitors to the SGP CART site are required to complete a Site Access Request (SAR) form before visiting the site.

49

ARM - PI Product - Aerosol Retrievals from ARM SGP MFRSR Data  

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ProductsAerosol Retrievals from ARM SGP MFRSR Data ProductsAerosol Retrievals from ARM SGP MFRSR Data Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send PI Product : Aerosol Retrievals from ARM SGP MFRSR Data 2000.01.01 - 2000.12.31 Site(s) SGP General Description The Multi-Filter Rotating Shadowband Radiometer (MFRSR) makes precise simultaneous measurements of the solar direct normal and diffuse horizontal irradiances at six wavelengths (nominally 415, 500, 615, 673, 870, and 940 nm) at short intervals (20 sec for ARM instruments) throughout the day. Time series of spectral optical depth are derived from these measurements. Besides water vapor at 940 nm, the other gaseous absorbers within the MFRSR channels are NO2 (at 415, 500, and 615 nm) and ozone (at 500, 615, and 670

50

knuteson-99.PDF  

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Observations at the ARM SGP, NSA, Observations at the ARM SGP, NSA, and TWP CART Sites R. O. Knuteson, H. E. Revercomb, F. A. Best, R. G. Dedecker, R. G. Garcia, H. B. Howell, D. C. Tobin, and V. P. Walden Space Science and Engineering Center University of Wisconsin Madison, Wisconsin Introduction A total of eight Atmospheric Emitted Radiance Interferometer (AERI) systems, developed at the University of Wisconsin-Madison Space Science and Engineering Center (UW-SSEC) for the measurement of the downwelling infrared radiance spectrum, have now been deployed at the Atmospheric Radiation Measurement (ARM) Program's Southern Great Plains (SGP), Tropical Western Pacific (TWP), and North Slope of Alaska (NSA) Cloud And Radiation Testbed (CART) sites (Revercomb 1993). In this paper we will review the status and recent results obtained from these AERI

51

* SGP Central Facility - surrounded by wheat felds, the  

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SGP Central Facility - surrounded by wheat felds, the SGP Central Facility - surrounded by wheat felds, the heavily instrumented Central Facility served as the primary source of information about cloud and carbon feedbacks. * Little Washita Watershed - located in a mix of pasture land and winter wheat, three carbon fux towers and associ ated instruments were added at this site. Two additional fux towers were located at Fort Cobb, in nearby croplands,

52

Observed Large-Scale Structures and Diabatic Heating and Drying Profiles during TWP-ICE  

Science Conference Proceedings (OSTI)

This study documents the characteristics of the large-scale structures and diabatic heating and drying profiles observed during the Tropical Warm PoolInternational Cloud Experiment (TWP-ICE), which was conducted in JanuaryFebruary 2006 in ...

Shaocheng Xie; Timothy Hume; Christian Jakob; Stephen A. Klein; Renata B. McCoy; Minghua Zhang

2010-01-01T23:59:59.000Z

53

ARM - PI Product - Cloud Properties and Radiative Heating Rates for TWP  

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ProductsCloud Properties and Radiative Heating Rates for ProductsCloud Properties and Radiative Heating Rates for TWP Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send PI Product : Cloud Properties and Radiative Heating Rates for TWP 2002.01.01 - 2012.02.08 Site(s) TWP General Description A cloud properties and radiative heating rates dataset is presented where cloud properties retrieved using lidar and radar observations are input into a radiative transfer model to compute radiative fluxes and heating rates at three ARM sites located in the Tropical Western Pacific (TWP) region. The cloud properties retrieval is a conditional retrieval that applies various retrieval techniques depending on the available data, that is if lidar, radar or both instruments detect cloud. This Combined Remote

54

A Comparison of the Water Budgets between Clouds from AMMA and TWP-ICE  

Science Conference Proceedings (OSTI)

Two field campaigns, the African Monsoon Multidisciplinary Analysis (AMMA) and the Tropical Warm PoolInternational Cloud Experiment (TWP-ICE), took place in 2006 near Niamey, Niger, and Darwin, Northern Territory, Australia, providing extensive ...

Xiping Zeng; Wei-Kuo Tao; Scott W. Powell; Robert A. Houze Jr.; Paul Ciesielski; Nick Guy; Harold Pierce; Toshihisa Matsui

2013-02-01T23:59:59.000Z

55

Continental Liquid-phase Stratus Clouds at SGP: Meteorological Influences  

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Continental Liquid-phase Stratus Clouds at SGP: Meteorological Influences Continental Liquid-phase Stratus Clouds at SGP: Meteorological Influences and Relationship to Adiabacity Kim, Byung-Gon Kangnung National University Schwartz, Stephen Brookhaven National Laboratory Miller, Mark Brookhaven National Laboratory Min, Qilong State University of New York at Albany Category: Cloud Properties The microphysical properties of continental stratus clouds observed over SGP appear to be substantially influenced by micrometeorological conditions, such as static stability and updraft velocity. These influences may contribute to the observed weak correlation of aerosol light scattering coefficient with cloud-drop effective radius [Kim et al., JGR, 2003], although aerosol light scattering coefficient is not necessarily the most suitable surrogate aerosol property for number concentration of cloud

56

ARM Carbon Cycle Gases Flasks at SGP Site  

DOE Data Explorer (OSTI)

Data from flasks are sampled at the Atmospheric Radiation Measurement Program ARM, Southern Great Plains Site and analyzed by the National Oceanic and Atmospheric Administration NOAA, Earth System Research Laboratory ESRL. The SGP site is included in the NOAA Cooperative Global Air Sampling Network. The surface samples are collected from a 60 m tower at the ARM SGP Central Facility, usually once per week in the afternoon. The aircraft samples are collected approximately weekly from a chartered aircraft, and the collection flight path is centered over the tower where the surface samples are collected. The samples are collected by the ARM and LBNL Carbon Project.

Sebastien Biraud

57

ARM Tropical Western Pacific (TWP) Operations Management and Support: Securing ARM Data  

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Tropical Western Pacific (TWP) Operations Tropical Western Pacific (TWP) Operations Management and Support: Securing ARM Data K. L. Nitschke South Pacific Regional Environment Programme Apia, Samoa L. Jones Los Alamos National Laboratory Los Alamos, New Mexico C. N. Long Pacific Northwest National Laboratory Richland, Washington Introduction The Tropical Western Pacific Office (TWPO) (a) has been tasked with providing operational management and support for three (b) climate station instrument facilities in the Tropical Western pacific (TWP) locale. The TWPO has the distinctive purview in ensuring data availability from two remote Pacific Islands and Australia to support the continued national and international scientific collaboration that exemplifies the Atmospheric Radiation Measurement (ARM) Program. Data from the international sites have been

58

Validation of Cloud Properties Derived from GOES-9 Over the ARM TWP Region  

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Cloud Properties Derived from Cloud Properties Derived from GOES-9 Over the ARM TWP Region M. M. Khaiyer, M. L. Nordeen, D. R. Doelling, and V. Chakrapani Analytical Services and Materials, Inc. Hampton, Virginia P. Minnis and W. L. Smith, Jr. Atmospheric Sciences National Aeronautic and Space Administration Langley Research Center Hampton, Virginia Introduction Satellite data are essential for monitoring clouds and radiative fluxes where ground-based instruments are unavailable. On April 24, 2003, the ninth geostationary operational environmental satellite (GOES-9) began operational coverage of the Tropical Western Pacific (TWP), replacing the failing fifth geostationary meteorological satellite (GMS-5). The GOES-9 imager provides the opportunity for enhanced monitoring of clouds and radiation over the TWP because it has better spatial resolution and

59

Using ARM TWP Nauru Observations to Evaluate a Simple Thermodynamic Model  

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Using ARM TWP Nauru Observations to Evaluate a Simple Thermodynamic Model Using ARM TWP Nauru Observations to Evaluate a Simple Thermodynamic Model of the Subcloud Layer Under Fair-Weather Cumulus Conditions Albrecht, Bruce University of Miami Kollias, Pavlos Brookhaven National Laboratory Category: Modeling Marine boundary layer clouds are fundamental in regulating the vertical structure of water vapor and entropy in the lowest 2 km of the Earth's atmosphere. The observations from the ARM TWP-Nauru site provide a unique opportunity to study these clouds and the associated boundary layer structure. In this study an atmospheric mixed layer representation of the subcloud layer for application in fair-weather cumulus regimes is used to develop a diagnostic model of the near surface temperature and moisture associated with a given surface temperature and wind speed. This model

60

New Eddy Correlation System for ARM SGP Site  

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New Eddy Correlation System for ARM SGP Site New Eddy Correlation System for ARM SGP Site M. S. Pekour Argonne National Laboratory Argonne, Illinois Background Eddy correlation (ECOR) systems are widely used for in situ measurement of the turbulent fluxes in the atmosphere. The ECOR technique is the most direct method for determining fluxes; vertical fluxes are obtained by correlating the vertical wind component with the horizontal wind component (momentum flux), temperature (sensible heat flux), water vapor density (latent heat flux), and a scalar admixture density (e.g., CO 2 flux). Typically, an ultrasonic anemometer-thermometer ("sonic anemometer") is used for rapid, high-precision, three-dimensional (3D) wind measurements, as well as for temperature fluctuation measurements. A fast-response humidity sensor, such as an infra-red gas analyzer (IRGA) is

Note: This page contains sample records for the topic "nsa sgp twp" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


61

Simultaneous Spectral Albedo Measurements Near the ARM SGP Central Facility  

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Simultaneous Spectral Albedo Measurements Simultaneous Spectral Albedo Measurements Near the ARM SGP Central Facility J. J. Michalsky and Q.-L. Min Atmospheric Sciences Research Center State University of New York Albany, New York J. C. Barnard and R. T. Marchand Pacific Northwest National Laboratory P. Pilewskie National Aeronautics and Space Administration Ames Research Center Moffett Field, California Introduction During ARM Enhanced Shortwave Experiment II (ARESE II) the Twin Otter aircraft made low-altitude (100-300-m) passes over the Central Facility (CF) at the Southern Great Plains (SGP) Clouds and Radiation Testbed (CART) site as part of the flight pattern design for the experiment. The National Aeronautics and Space Administration (NASA) Ames Research Center's Solar Spectral Flux

62

Direct Aerosol Forcing in the Infrared at the SGP Site?  

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Direct Aerosol Forcing in the Infrared at the SGP Site? Direct Aerosol Forcing in the Infrared at the SGP Site? D. D. Turner and C. N. Long Pacific Northwest National Laboratory Richland, Washington Introduction Low level haze is often observed during the night and early morning hours in many locations. This haze is typically formed during quiescent conditions by radiative cooling of the surface, which lowers the ambient temperature and consequently increases the near-surface relative humidity (RH). Many aerosols start to deliquesce around 75% relative humidity (RH) (depending on their chemical composition), and thus if the near surface RH increases above this level, haze will form. The Atmospheric Radiation Measurement (ARM) Program's ultimate goal, stated simply, is to improve the treatment of radiative transfer in global climate models. Global climate models typically do not

63

SGP Cloud and Land Surface Interaction Campaign (CLASIC): Measurement Platforms  

SciTech Connect

The Cloud and Land Surface Interaction Campaign (CLASIC) will be conducted from June 8 to June 30, 2007, at the U.S. Department of Energys Atmospheric Radiation Measurement (ARM) Climate Research Facility (ACRF) Southern Great Plains (SGP) site. Data will be collected using eight aircraft equipped with a variety of specialized sensors, four specially instrumented surface sites, and two prototype surface radar systems. The architecture of CLASIC includes a high-altitude surveillance aircraft and enhanced vertical thermodynamic and wind profile measurements that will characterize the synoptic scale structure of the clouds and the land surface within the ACRF SGP site. Mesoscale and microscale structures will be sampled with a variety of aircraft, surface, and radar observations. An overview of the measurement platforms that will be used during the CLASIC are described in this report. The coordination of measurements, especially as it relates to aircraft flight plans, will be discussed in the CLASIC Implementation Plan.

MA Miller; R Avissar; LK Berg; SA Edgerton; ML Fischer; TJ Jackson; B. Kustas; PJ Lamb; G McFarquhar; Q Min; B Schmid; MS Torn; DD Tuner

2007-06-01T23:59:59.000Z

64

Anvil Characteristics as Seen by C-POL during the Tropical Warm Pool International Cloud Experiment (TWP-ICE)  

Science Conference Proceedings (OSTI)

The Tropical Pacific Warm Pool International Cloud Experiment (TWP-ICE) took place in Darwin, Australia, in early 2006. C-band radar data were used to characterize tropical anvil (i.e., thick, nonprecipitating cloud associated with deep ...

Kaycee Frederick; Courtney Schumacher

2008-01-01T23:59:59.000Z

65

Progress on an ARM/GCSS/SPARC TWP-ICE Monsoon Case Study  

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Progress Progress on an ARM/GCSS/SPARC TWP-ICE Monsoon Case Study Ann Fridlind and Andrew Ackerman ann.fridlind@nasa.gov * www.giss.nasa.gov/∼fridlind Introduction Source: Lori Chappel, Australian BOM The Tropical Warm Pool-International Cloud Experiment (TWP-ICE) assembled aircraft and ground instruments at the DOE-ARM long-term site in Darwin, Australia during the 2005/2006 monsoon, and the early part of the campaign encountered active monsoon conditions (left). The goal of this work is to help develop a model intercomparison case study that can be carried out jointly by three organizations: the ARM cloud modeling working group, the GEWEX Cloud System Study (GCSS) deep convective clouds group, and the Stratospheric Processes and Their Role in Climate (SPARC) group. Case description ◮ idealized maritime convection (specified SST) ◮ large-scale forcing data from

66

Radiation Dry Bias in the TWP-ICE Radiosonde Soundings Solar Zenith Angle Correction Factor  

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Radiation Dry Bias in the TWP-ICE Radiosonde Soundings Radiation Dry Bias in the TWP-ICE Radiosonde Soundings Solar Zenith Angle Correction Factor Figure 3: Ratio of MWR TCWV to radiosonde derived TCWV, and the solar zenith angle at the radiosonde launch time (black dots). The dry bias observed in sonde TCWV values is mainly attributable to a dry RH bias near the surface The red dots show the 1000 hPa RH correction factors suggested by Voemel et al for sondes launched near noon (10-30 degree solar zenith angle), and at night time (90 degree zenith angle). The green line shows a modified RH correction factor which is a function of the solar zenith angle. ● During the day-time, the TCWV bias is significantly smaller when the zenith angle correction is applied than when no correction, or only the Crad and Ccal corrections are applied.

67

TWP-ICE Data from the GEWEX Cloud System Study: Data Integration for Model Evaluation (GCSSDIME)  

DOE Data Explorer (OSTI)

One of the most complete data sets of tropical cirrus and convection observations resulted from the Tropical Warm Pool - International Cloud Experiment (TWP-ICE) in the area around Darwin, Australia. The aim of the experiment is to examine convective cloud systems from their initial stages through the decaying and thin high level cirrus and measure their impact on the environment. The experiment design includes an unprecedented array of soundings and other information to support cloud resolving and other modeling studies as well as a large range of in-situ and remotely sensed observation platforms. A key component of the field campaign is a fleet of aircraft including the Dornier, Dimona, Egrett, Twin Otter, and Proteus. Together, these aircraft collected measurements of cloud properties and the meteorological environment from the planetary boundary layer up to 15 km high. The extensive ground network of cloud sensing radar, lidar and passive instruments are located on a ship and several ground sites throughout the experimental domain. This case study presents data from 19 Jan 2006 to 28 Feb 2006 and covers a region from 25S to 10S latitude and from 125E to 140E longitude.[Copied from http://gcss-dime.giss.nasa.gov/twp-ice/twp-ice.html

68

CIMEL Measurements of Zenith Radiances at the ARM SGP Site  

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CIMEL Measurements of Zenith Radiances CIMEL Measurements of Zenith Radiances at the ARM SGP Site W. J. Wiscombe National Aeronautics and Space Administration Goddard Space Flight Center Climate and Radiation Branch Greenbelt, Maryland A. Marshak and K. Evans Joint Center for Earth Systems Technology University of Maryland Baltimore, Maryland Y. Knyazikhin Department of Geography Boston University Boston, Massachusetts H. W. Barker Environment Canada Downsview, Ontario, Canada C. F. Pavloski Department of Meteorology Pennsylvania State University University Park, Pennsylvania A. B. Davis Los Alamos National Laboratory Space and Remote Sensing Sciences Los Alamos, New Mexico M. Miller Brookhaven National Laboratory Upton, New York Introduction The objective of our study is to exploit the sharp spectral contrast in vegetated surface reflectance across

69

SGP Cloud and Land Surface Interaction Campaign (CLASIC)  

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3 3 SGP Cloud and Land Surface Interaction Campaign (CLASIC): Science and Implementation Plan June 2007 Mark A. Miller, Principal Investigator and The CLASIC Steering Committee: Roni Avissar, Larry Berg, Sylvia Edgerton, Marc Fischer, Tom Jackson, Bill Kustas, Pete Lamb, Greg McFarquhar, Qilong Min, Beat Schmid, Margaret Torn, and Dave Turner Work supported by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research M.R. Miller et al., DOE/SC-ARM-0703 Executive Summary The Cloud and Land Surface Interaction Campaign is a field experiment designed to collect a comprehensive data set that can be used to quantify the interactions that occur between the atmosphere, biosphere, land surface, and subsurface. A particular focus will be on how these

70

ARM - Field Campaign - Ground-based Cloud Tomography Experiment at SGP  

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govCampaignsGround-based Cloud Tomography Experiment at SGP govCampaignsGround-based Cloud Tomography Experiment at SGP Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Campaign : Ground-based Cloud Tomography Experiment at SGP 2009.05.26 - 2009.07.17 Lead Scientist : Dong Huang For data sets, see below. Description Knowledge of 3D cloud properties is pressingly needed in many research fields. One of the problems encountered when trying to represent 3D cloud fields in numerical models is that the existing techniques cannot provide necessary observations at the required spatial scale and resolution. We tested a new promising technique for measuring 3D cloud microphysical structure, called cloud microwave tomography, at the Southern Great Plains (SGP) site for one month in late April 2009. Five microwave scanning

71

Evaluation of Precipitation Simulated by Seven SCMs against the ARM Observations at the SGP Site  

Science Conference Proceedings (OSTI)

This study evaluates the performances of seven single-column models (SCMs) by comparing simulated surface precipitation with observations at the Atmospheric Radiation Measurement Program Southern Great Plains (SGP) site from January 1999 to ...

Hua Song; Wuyin Lin; Yanluan Lin; Audrey B. Wolf; Roel Neggers; Leo J. Donner; Anthony D. Del Genio; Yangang Liu

2013-08-01T23:59:59.000Z

72

Using a Microwave Emission Model to Estimate Soil Moisture from ESTAR Observations during SGP99  

Science Conference Proceedings (OSTI)

The 1999 Southern Great Plains Hydrology Experiment (SGP99) provides comprehensive datasets for evaluating microwave remote sensing of soil moisture algorithms that involve complex physical properties of soils and vegetation. The Land Surface ...

Huilin Gao; Eric F. Wood; Matthias Drusch; Wade Crow; Thomas J. Jackson

2004-02-01T23:59:59.000Z

73

Climatology of Warm Boundary Layer Clouds at the ARM SGP Site and Their Comparison to Models  

Science Conference Proceedings (OSTI)

A 4-yr climatology (19972000) of warm boundary layer cloud properties is developed for the U.S. Department of Energy Atmospheric Radiation Measurement (ARM) Program Southern Great Plains (SGP) site. Parameters in the climatology include cloud ...

Manajit Sengupta; Eugene E. Clothiaux; Thomas P. Ackerman

2004-12-01T23:59:59.000Z

74

Assessment of the ECMWF Model Cloudiness and Surface Radiation Fields at the ARM SGP Site  

Science Conference Proceedings (OSTI)

The cloud and radiation fields produced by the operational ECMWF forecasts are assessed using observations from the Atmospheric Radiation Measurement Program (ARM) Southern Great Plains (SGP) site over the AprilMay 1999 period. Over the first 36 ...

Jean-Jacques Morcrette

2002-02-01T23:59:59.000Z

75

ARM - Evaluation Product - Landsat Thematic Mapper (TM)  

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ProductsLandsat Thematic Mapper (TM) ProductsLandsat Thematic Mapper (TM) Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Evaluation Product : Landsat Thematic Mapper (TM) Site(s) NSA SGP TWP General Description The Landsat satellites are used to acquire remotely sensed images of the Earth's land surface and surrounding coastal regions. The Landsat-5 TM files are binary. In addition, some of the Landsat-5 TM files were sent to the Archive in exported form from ArcInfo (GIS software). The Landsat-7 TM files are HDF. These files are delivered to the archive as tarred files and include documentation. Landsat-5 TM satellite data scenes are available for the NSA and SGP sites. In addition, Landsat-7 satellite data scenes are available for the SGP and

76

Cumulus Geometry from Satellite and Surface Data at the ARM TWP Site  

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Cumulus Geometry from Satellite and Surface Data Cumulus Geometry from Satellite and Surface Data at the ARM TWP Site E. I. Kassianov, T. P. Ackerman, and R. T. Marchand Pacific Northwest National Laboratory Richland, Washington Introduction The multi-angle imaging spectrometer (MISR), a sensor on board the earth observing system (EOS) Terra satellite platform, observes reflected radiation in nine directions with high resolution (~0.275 km). The overall mission of the MISR is to provide continuous, global multi-angle measurements of the reflected radiation from the earth's atmosphere and surface, and thereby create a valuable resource for studying their physical properties (Diner et al. 1999). For single-layer marine cumulus clouds, we have demonstrated that satellite-derived basic statistics (mean, variance) of vertical cloud size match closely

77

How Representative are the Cloud Regimes at the TWP Sites? … An ISCCP Perspective  

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How Representative are the Cloud Regimes at the How Representative are the Cloud Regimes at the TWP Sites? - An ISCCP Perspective C. Jakob Bureau of Meteorology Research Centre Melbourne, Australia G. Tselioudis National Aeronautic and Space Administration Goddard Institute for Space Studies Columbia University New York Introduction The Atmospheric Radiation Measurement (ARM) Program has established comprehensive cloud and radiation observatories in various locations across the globe with the aim of collecting measurements and developing models to better understand the processes that control solar and thermal infrared radiative transfer in clouds and at the surface. The locales of the individual ARM sites were chosen because they represent typical cloud regimes occurring in various climate regimes (Stokes and Schwartz

78

The Status and Future of AERIs in ARM  

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Status and Future of AERIs Status and Future of AERIs in ARM Dave Turner Space Science and Engineering Center University of Wisconsin - Madison Longwave/Microwave Focus Group 11 March 2008 ARM STM, Norfolk, VA Background * Spectrally resolved IR radiances were considered key component of ARM's observational strategy * Stringent requirements placed on absolute radiometric accuracy (1% ambient radiance), spectral accuracy, noise level, and operability * Instrument development was successful! * ARM has 8 AERI systems: * 11 Million calibrated sky spectra have been collected by ARM AERIs (up to Dec 2007) * SGP-01 * SGP-E14 * AMF-M1 * NSA-C1 (ER) * TWP-C2 * TWP-C3 * Spare (NR) * Spare (ER) AERI Interferometer Assembly AERI Interferometer Assembly Bomem Interferometer ABB HBB Optics Optics Bench Bench Shock

79

Derivation of Seasonal Cloud Properties at ARM-NSA from Multispectral MODIS Data  

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Derivation of Seasonal Cloud Properties at ARM-NSA Derivation of Seasonal Cloud Properties at ARM-NSA from Multispectral MODIS Data D. A. Spangenberg Analytical Services and Materials, Inc. Hampton, Virginia P. Minnis National Aeronautics and Space Administration Langley Research Center Hampton, Virginia T. Uttal National Oceanic and Atmospheric Administration Environmental Technology Laboratory Boulder, Colorado Q. Z. Trepte and S. S.-Mack Science Applications International Corporation Hampton, Virginia Introduction Improving climate model predictions over earth's Polar Regions requires a complete knowledge of polar cloud microphysics. Over the Arctic, there is minimal contrast between the clouds and background snow surface observed in satellite data, especially for visible wavelengths. This makes it difficult to

80

Analysis of Selected Radiosonde Data from the ARM/NSA Site  

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Analysis of Selected Radiosonde Data Analysis of Selected Radiosonde Data from the ARM/NSA Site B. Petracca, H. W. Church, and B. D. Zak Sandia National Laboratories Albuquerque, New Mexico R. Storvold and C. Marty Geophysical Institute University of Alaska Fairbanks, Alaska B. M. Lesht Argonne National Laboratories Argonne, Illinois Introduction The purpose of this study was to analyze differences in temperature and relative humidity (RH) profiles obtained from near-simultaneous radiosonde soundings made from different locations at and near the North Slope of Alaska (NSA) Cloud and Radiation Testbed (CART) site. The data for this study come from the Vaisala RS-80H radiosondes flown by Atmospheric Radiation Measurement (ARM) Program during the comparison periods, and from VIZ B2 radiosondes flown by the National Weather Service

Note: This page contains sample records for the topic "nsa sgp twp" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


81

ARM Quick-looks Database for North Slope Alaska (NSA) sites  

DOE Data Explorer (OSTI)

From these pages one can monitor parts of the data acquisition process and access daily data visualizations from the different instruments. These data visualizations are produced in near real time automatically and are called Quick-Looks (QLs). The quick-looks contains unofficial data of unknown quality. Once data is released one can obtain the full data-set from any instrument available, and along with that, a statement about the data quality from the ARM archive. The database provides Quick-looks for the Barrow ACRF site (NSA C1), the Atqasuk ACRF site (NSA C2), or the SHEBA ice campaign of 1997 and 1998. As of 12-17-08, the database had more than 528,000 quick-looks available as data figures and data plots. No password is required for Quick-look access. (Specialized Interface)

Stamnes, Knut (NSA Site Scientist)

82

ARM - VAP Product - armbecldrad  

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Productsarmbearmbecldrad Productsarmbearmbecldrad Documentation Data Management Facility Plots (Quick Looks) Citation DOI: 10.5439/1095314 DOI: 10.5439/1039926 Central Facility, Lamont, OK (SGP C1) DOI: 10.5439/1039927 Central Facility, Barrow AK (NSA C1) DOI: 10.5439/1039928 Central Facility, Manus I., PNG (TWP C1) DOI: 10.5439/1039929 Central Facility, Nauru Island (TWP C2) DOI: 10.5439/1039930 Central Facility, Darwin, Australia (TWP C3) [ What is this? ] Generate Citation ARM Data Discovery Browse Data Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send VAP Output : ARMBECLDRAD ARMBE: Cloud Radiation measurements Active Dates 1996.01.01 - 2011.01.01 Originating VAP Process ARM Best Estimate Data Products : ARMBE Description The ARMBE Cloud Radiation (ARMBECLDRAD) VAP contains a best estimate of

83

ARM - VAP Product - armbeatm  

NLE Websites -- All DOE Office Websites (Extended Search)

Productsarmbearmbeatm Productsarmbearmbeatm Documentation Data Management Facility Plots (Quick Looks) Citation DOI: 10.5439/1095313 DOI: 10.5439/1039931 Central Facility, Lamont, OK (SGP C1) DOI: 10.5439/1039932 Central Facility, Barrow AK (NSA C1) DOI: 10.5439/1039933 Central Facility, Manus I., PNG (TWP C1) DOI: 10.5439/1039934 Central Facility, Nauru Island (TWP C2) DOI: 10.5439/1039935 Central Facility, Darwin, Australia (TWP C3) [ What is this? ] Generate Citation ARM Data Discovery Browse Data Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send VAP Output : ARMBEATM ARMBE: Atmospheric measurements Active Dates 1994.01.01 - 2012.12.31 Originating VAP Process ARM Best Estimate Data Products : ARMBE Description The ARM Best Estimate Atmospheric Measurements (ARMBEATM) value-added

84

A Comparison of TWP-ICE Observational Data with Cloud-Resolving Model Results  

SciTech Connect

Observations made during the TWP-ICE campaign are used to drive and evaluate thirteen cloud-resolving model simulations with periodic lateral boundary conditions. The simulations employ 2D and 3D dynamics, one- and two-moment microphysics, several variations on large-scale forcing, and the use of observationally derived aerosol properties to prognose droplet numbers. When domain means are averaged over a 6-day active monsoon period, all simulations reproduce observed surface precipitation rate but not its structural distribution. Simulated fractional areas covered by convective and stratiform rain are uncorrelated with one another, and are both variably overpredicted by up to a factor of {approx}2. Stratiform area fractions are strongly anticorrelated with outgoing longwave radiation (OLR) but are negligibly correlated with ice water path (IWP), indicating that ice spatial distribution controls OLR more than mean IWP. Overpredictions of OLR tend to be accompanied by underpredictions of reflected shortwave radiation (RSR). When there are two simulations differing only in microphysics scheme or large-scale forcing, the one with smaller stratiform area tends to exhibit greater OLR and lesser RSR by similar amounts. After {approx}10 days, simulations reach a suppressed monsoon period with a wide range of mean precipitable water vapor, attributable in part to varying overprediction of cloud-modulated radiative flux divergence compared with observationally derived values. Differences across the simulation ensemble arise from multiple sources, including dynamics, microphysics, and radiation treatments. Close agreement of spatial and temporal averages with observations may not be expected, but the wide spreads of predicted stratiform fraction and anticorrelated OLR indicate a need for more rigorous observation-based evaluation of the underlying micro- and macrophysical properties of convective and stratiform structures.

Fridlind, A. M.; Ackerman, Andrew; Chaboureau, Jean-Pierre; Fan, Jiwen; Grabowski, Wojciech W.; Hill, A.; Jones, T. R.; Khaiyer, M. M.; Liu, G.; Minnis, Patrick; Morrison, H.; Nguyen, L.; Park, S.; Petch, Jon C.; Pinty, Jean-Pierre; Schumacher, Courtney; Shipway, Ben; Varble, A. C.; Wu, Xiaoqing; Xie, Shaocheng; Zhang, Minghua

2012-03-13T23:59:59.000Z

85

TWP-ICE Global Atmospheric Model Intercomparison: Convection Responsiveness and Resolution Impact  

SciTech Connect

Results are presented from an intercomparison of global atmospheric model (GAM) simulations of tropical convection during the Tropical Warm Pool-International Cloud Experiment (TWP-ICE). The distinct cloud properties, precipitation, radiation, and vertical diabatic heating profiles associated with three different monsoon regimes (wet, dry, and break) from available observations are used to evaluate 9 GAM forecasts initialized daily from realistic global analyses. All models well captured the evolution of large-scale circulation and the thermodynamic fields, but cloud properties differed substantially among models. For example, liquid water path and ice water path differed by up to two orders of magnitude. Compared with the relatively well simulated top-heavy heating structures during the wet and break period, most models had difficulty in depicting the bottom-heavy heating profiles associated with cumulus congestus. The best performing models during this period were the ones whose convection scheme was most responsive to the free tropospheric humidity. Compared with the large impact of cloud and convective parameterizations on model cloud and precipitation characteristics, resolution has relatively minor impact on simulated cloud properties. However, one feature that was influence by the resolution study in several models was the diurnal cycle of precipitation. Peaking at a different time from convective precipitation, large-scale precipitation generally increases in high resolution forecasts and modulates the total precipitation diurnal cycle. Overall, the study emphasizes the importance of more environmental responsive convective parameterizations to capture various types of convection and the substantial diversity among large-scale cloud and precipitation schemes in current GAMs. This experiment has also demonstrated itself to be a very useful testbed for those developing cloud and convection schemes in these models.

Lin, Yanluan; Donner, Leo J.; Petch, Jon C.; Bechtold, P.; Boyle, James; Klein, Stephen A.; Komori, T.; Wapler, K.; Willett, M.; Xie, X.; Zhao, M.; Xie, Shaocheng; McFarlane, Sally A.; Schumacher, Courtney

2012-05-08T23:59:59.000Z

86

Improved ARM-SGP TOA OLR Fluxes from GOES-8 IR Radiances Based on CERES Data  

NLE Websites -- All DOE Office Websites (Extended Search)

ARM-SGP TOA OLR Fluxes from GOES-8 IR ARM-SGP TOA OLR Fluxes from GOES-8 IR Radiances Based on CERES Data D. R. Doelling and M. M. Khaiyer Analytical Services and Materials, Inc. Hampton, Virginia P. Minnis National Aeronautics and Space Administration Langley Research Center Hampton, Virginia Introduction The radiation budget at the top of the atmosphere (TOA) is a quantity of fundamental importance to the Atmospheric Radiation Measurement (ARM) Program. Thus, it is necessary to measure the radiation budget components, broadband shortwave albedo and outgoing longwave radiation (OLR), as accurately as possible. Measurement of OLR over the ARM surface sites has only been possible since the advent of Clouds and the Earth's Radiant Energy System (CERES; Wielicki et al. 1998) in 1998. Prior to

87

Infrared Land Surface Emissivity in the Vicinity of the ARM SGP Central Facility  

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Infrared Land Surface Emissivity in the Vicinity Infrared Land Surface Emissivity in the Vicinity of the ARM SGP Central Facility R. O. Knuteson, R. G. Dedecker, W. F. Feltz, B. J. Osbourne, H. E. Revercomb, and D. C. Tobin Space Science and Engineering Center University of Wisconsin-Madison Madison, Wisconsin Introduction The University of Wisconsin Space Science and Engineering Center (UW-SSEC) has developed, under National Aeronautics and Space Administration (NASA) funding, a model for the infrared land surface emissivity (LSE) in the vicinity of the U.S. Department of Energy's (DOE) Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) Cloud and Radiation Testbed (CART) Central Facility (CF) in North Central Oklahoma. The UW-Madison LSE model is part of the ARM best

88

Determination of Ice Water Path Over the ARM SGP Using Combined Surface and Satellite Datasets  

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Determination of Ice Water Path Over the ARM SGP Using Determination of Ice Water Path Over the ARM SGP Using Combined Surface and Satellite Datasets J. Huang, M. M. Khaiyer, and P. W. Heck Analytical Services & Materials, Inc. Hampton, Virginia P. Minnis and B. Lin Atmospheric Sciences National Aeronautics and Space Administration Langley Research Center Hampton, Virginia T.-F. Fan Science Applications International Corporation Hampton, Virginia Introduction Global information of cloud ice water path (IWP) is urgently needed for testing of global climate models (GCMs) and other applications. Accurate quantification of the IWP is essential for characterizing the hydrological and radiation budget. For example, the reflection of shortwave radiation by ice clouds reduces the solar energy reaching the earth's surface. Ice clouds can also trap the longwave radiation

89

Searching for Global Dimming Evidence at SGP and Update of ARM Submissions to BSRN  

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Searching for Global Dimming Evidence at SGP and Searching for Global Dimming Evidence at SGP and Update of ARM Submissions to BSRN G. Hodges Cooperative Institute for Research in Environmental Sciences University of Colorado Boulder, Colorado Introduction Global dimming, usually defined as a reduction of incoming solar radiation (insolation) at the surface of the earth, is a topic being discussed with increasing frequency. A recent news article on global dimming in the web-based newspaper the Guardian Unlimited seems to have brought this issue to the forefront with scientists and laypeople alike. In fact, there is a special session devoted to global dimming at the upcoming May 17-21 American Geophysical Union (AGU) meeting in Montreal, Canada. The article quotes Atsumu Ohmura and references his findings on this subject.

90

Verification of Patch- and Regional-Scale Energy Balance Estimates Derived from Microwave and Optical Remote Sensing during SGP97  

Science Conference Proceedings (OSTI)

The 1997 Southern Great Plains Hydrology Experiment (SGP97) was designed and conducted to extend surface soil moisture retrieval algorithms based on passive microwave observations to coarser resolutions, larger regions with more diverse ...

William P. Kustas; Thomas J. Jackson; Andrew N. French; J. Ian MacPherson

2001-06-01T23:59:59.000Z

91

A Climatology of Midlatitude Continental Clouds from the ARM SGP Central Facility. Part II: Cloud Fraction and Surface Radiative Forcing  

Science Conference Proceedings (OSTI)

Data collected at the Department of Energy Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) Central Facility (SCF) are analyzed to determine the monthly and hourly variations of cloud fraction and radiative forcing between ...

Xiquan Dong; Baike Xi; Patrick Minnis

2006-05-01T23:59:59.000Z

92

Evaluating Deep Updraft Formulation in NCAR CAM3 with High-Resolution WRF Simulations During ARM TWP-ICE  

SciTech Connect

The updraft formulation used in NCAR CAM3 deep convection parameterization assumes that the fractional entrainment rate for a single updraft is height-independent and the updraft mass flux increases monotonically with height to updraft top. These assumptions are evaluated against three-dimensional high-resolution simulations from the weather research and forecast (WRF) model during the monsoon period of the DOE ARM Tropical Warm Pool -- International Cloud Experiment (TWP-ICE). Analyses of the WRF-generated updrafts suggest that the fractional entrainment rate for a single updraft decreases with height and the updraft mass flux increases with height below the top of the conditionally unstable layer but decreases above. It is suggested that the assumed updraft mass flux profile in CAM3 might be unrealistic in many cases because the updraft acceleration is affected by other drag processes in addition to entrainment. Total convective cloud mass flux and detrainment rate over the TWP-ICE domain diagnosed from the CAM3 parameterization driven by WRF meteorological fields are smaller than those derived from WRF simulations. The total entrainment rate of CAM3 is smaller than that of WRF in the lower part of cloud and larger in the upper part of cloud. Compared with WRF simulations, the CAM3-parameterized convection is too active and, as a result, excess moisture and heat may be transported to the upper troposphere by the parameterized convection. Future improvement is envisioned.

Wang, Weiguo; Liu, Xiaohong

2009-02-19T23:59:59.000Z

93

halthore(3)-99.PDF  

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Sun and Sky Radiometric Measurements at the Sun and Sky Radiometric Measurements at the CART ARM SGP Site R. N. Halthore, S. E. Schwartz, Y. Liu, and P. H. Daum Brookhaven National Laboratory Upton, New York B. N. Holben National Aeronautics and Space Administration Goddard Space Flight Center Greenbelt, Maryland J. J. Michalsky State University of New York Albany, New York Abstract Cimel sunphotometers/radiometers (CSPHOT) are facility instruments at the three Atmospheric Radiation Measurement (ARM) sites at the Southern Great Plains (SGP) in Oklahoma, Tropical Western Pacific (TWP) in Nauru, and North Slope in Alaska (NSA). Here inferred aerosol optical thickness (AOT) and precipitable water (PW) measurements at the SGP site are compared with measurements using other instruments. Aerosol size distribution derived from direct solar measurements and from the

94

Nuclear science abstracts (NSA) database 1948--1974 (on the Internet)  

SciTech Connect

Nuclear Science Abstracts (NSA) is a comprehensive abstract and index collection of the International Nuclear Science and Technology literature for the period 1948 through 1976. Included are scientific and technical reports of the US Atomic Energy Commission, US Energy Research and Development Administration and its contractors, other agencies, universities, and industrial and research organizations. Coverage of the literature since 1976 is provided by Energy Science and Technology Database. Approximately 25% of the records in the file contain abstracts. These are from the following volumes of the print Nuclear Science Abstracts: Volumes 12--18, Volume 29, and Volume 33. The database contains over 900,000 bibliographic records. All aspects of nuclear science and technology are covered, including: Biomedical Sciences; Metals, Ceramics, and Other Materials; Chemistry; Nuclear Materials and Waste Management; Environmental and Earth Sciences; Particle Accelerators; Engineering; Physics; Fusion Energy; Radiation Effects; Instrumentation; Reactor Technology; Isotope and Radiation Source Technology. The database includes all records contained in Volume 1 (1948) through Volume 33 (1976) of the printed version of Nuclear Science Abstracts (NSA). This worldwide coverage includes books, conference proceedings, papers, patents, dissertations, engineering drawings, and journal literature. This database is now available for searching through the GOV. Research Center (GRC) service. GRC is a single online web-based search service to well known Government databases. Featuring powerful search and retrieval software, GRC is an important research tool. The GRC web site is at http://grc.ntis.gov.

NONE

1999-02-01T23:59:59.000Z

95

Characterizing the Vertical Distribution of Aerosols Over the ARM SGP Site  

Science Conference Proceedings (OSTI)

This project focused on: 1) evaluating the performance of the DOE ARM SGP Raman lidar system in measuring profiles of water vapor and aerosols, and 2) the use of the Raman lidar measurements of aerosol and water vapor profiles for assessing the vertical distribution of aerosols and water vapor simulated by global transport models and examining diurnal variability of aerosols and water vapor. The highest aerosol extinction was generally observed close to the surface during the nighttime just prior to sunrise. The high values of aerosol extinction are most likely associated with increased scattering by hygroscopic aerosols, since the corresponding average relative humidity values were above 70%. After sunrise, relative humidity and aerosol extinction below 500 m decreased with the growth in the daytime convective boundary layer. The largest aerosol extinction for altitudes above 1 km occurred during the early afternoon most likely as a result of the increase in relative humidity. The water vapor mixing ratio profiles generally showed smaller variations with altitude between day and night. We also compared simultaneous measurements of relative humidity, aerosol extinction, and aerosol optical thickness derived from the ARM SGP Raman lidar and in situ instruments on board a small aircraft flown routinely over the ARM SGP site. In contrast, the differences between the CARL and IAP aerosol extinction measurements are considerably larger. Aerosol extinction derived from the IAP measurements is, on average, about 30-40% less than values derived from the Raman lidar. The reasons for this difference are not clear, but may be related to the corrections for supermicron scattering and relative humidity that were applied to the IAP data. The investigators on this project helped to set up a major field mission (2003 Aerosol IOP) over the DOE ARM SGP site. One of the goals of the mission was to further evaluate the aerosol and water vapor retrievals from this lidar system. Analysis of the aerosol and water vapor data collected by the Raman lidar during the 2003 Aerosol IOP indicated that the sensitivity of the lidar was significantly lower than when the lidar was initially deployed. A detailed analysis after the IOP of the long-term dataset demonstrated that the lidar began degrading in early 2002, and that it lost approximately a factor of 4 in sensitivity between 2002 and 2004. We participated in the development of the remediation plan for the system to restore its initial performance. We conducted this refurbishment and upgrade from May- September 2004. This remediation lead to an increase in the signal-to-noise ratio of 10 and 30 for the Raman lidar's water vapor mixing ratio and aerosol backscatter coefficient data, respectively as compared to the signal strengths when the system was first deployed. The DOE ARM Aerosol Lidar Validation Experiment (ALIVE), which was conducted during September 2005, evaluated the impact of these modifications and upgrades on the SGP Raman lidar measurements of aerosol extinction and optical thickness. The CARL modifications significantly improved the accuracy and temporal resolution of the aerosol measurements. Aerosol extinction profiles measured by the Raman lidar were also used to evaluate aerosol extinction profiles and aerosol optical thickness (AOT) simulated by aerosol models as part of the Aerosol module inter-Comparison in global models (AEROCOM) (http://nansen.ipsl.jussieu.fr/AEROCOM/aerocomhome.html) project. There was a wide range in how the models represent the aerosol extinction profiles over the ARM SGP site, even though the average annual AOT represented by the various models and measured by CARL and the Sun photometer were in general agreement, at least within the standard deviations of the averages. There were considerable differences in the average vertical distributions among the models, even among models that had similar average aerosol optical thickness. Deviations between mean aerosol extinction profiles were generally small (~20-30%) for altitudes above 2 km, and grew consider

Richard Ferrare, Connor Flynn, David Turner

2009-05-05T23:59:59.000Z

96

ARM - Instrument Location Table  

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govInstrumentsLocation Table govInstrumentsLocation Table Instruments Location Table Contacts Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Instrument Locations Site abbreviations explained in the key. Instrument Name Abbreviation NSA SGP TWP AMF C1 C2 EF BF CF EF IF C1 C2 C3 EF IF Aerosol Chemical Speciation Monitor ACSM Atmospheric Emitted Radiance Interferometer AERI Aethalometer AETH Ameriflux Measurement Component AMC Aerosol Observing System AOS Meteorological Measurements associated with the Aerosol Observing System AOSMET Broadband Radiometer Station BRS

97

Surface Energy Balance System (SEBS) Handbook  

Science Conference Proceedings (OSTI)

A Surface Energy Balance System (SEBS) has been installed collocated with each deployed ECOR system at the Southern Great Plains (SGP), North Slope of Alaska (NSA), Tropical Western Pacific (TWP), ARM Mobile Facility 1 (AMF1), and ARM Mobile Facility 2 (AMF2). The surface energy balance system consists of upwelling and downwelling solar and infrared radiometers within one net radiometer, a wetness sensor, and soil measurements. The SEBS measurements allow the comparison of ECOR sensible and latent heat fluxes with the energy balance determined from the SEBS and provide information on wetting of the sensors for data quality purposes.

Cook, DR

2011-02-14T23:59:59.000Z

98

Observed and Simulated Cirrus Cloud Properties at the SGP CART Site  

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and Simulated Cirrus Cloud Properties and Simulated Cirrus Cloud Properties at the SGP CART Site A. D. Del Genio and A. B. Wolf National Aeronautics and Space Administration Goddard Institute for Space Studies New York, New York G. G. Mace University of Utah Salt Lake City, Utah Introduction Despite their potential importance in a long-term climate change, less is known about cirrus clouds than most other cloud types, for a variety of reasons (Del Genio 2001) including: (1) the difficulty of remotely sensing ice water content (IWC), (2) uncertainty in the identities of ice nuclei and the relative importance of different nucleation processes, (3) significant variations in depth and optical thickness caused by formation and sedimentation of large particles, and (4) our relatively poor documentation of

99

Validation of Satellite-Derived Liquid Water Paths Using ARM SGP Microwave Radiometers  

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Satellite-Derived Liquid Water Paths Using Satellite-Derived Liquid Water Paths Using ARM SGP Microwave Radiometers M. M. Khaiyer and J. Huang Analytical Services & Materials, Inc. Hampton, Virginia P. Minnis, B. Lin, and W. L. Smith, Jr. National Aeronautics and Space Administration Langley Research Center Hampton, Virginia A. Fan Science Applications International Corporation Hampton, Virginia A. Rapp Colorado State University Fort Collins, Colorado Introduction Satellites are useful for monitoring climatological parameters over large domains. They are especially useful for measuring various cloud microphysical and radiative parameters where ground-based instruments are not available. The geostationary operational environmental satellite (GOES) has been used to retrieve cloud and radiative properties over an extended domain centered on the Atmospheric

100

Techniques and Methods Used to Determine the Best Estimate of Radiation Fluxes at SGP Central Facility  

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Techniques and Methods Used to Determine the Techniques and Methods Used to Determine the Best Estimate of Radiation Fluxes at SGP Central Facility Y. Shi and C. N. Long Pacific Northwest National Laboratory Richland, Washington Algorithm and Methodology The Best Estimate Flux value-added product (VAP) processes data started on March 22, 1997, when data from the three central facility (CF) radiometer systems, Solar Infrared Station (SIRS) E13, C1, and baseline surface radiation network (BSRN) (sgpsirs1duttE13.c1, sgpsirs1duttC1.c1, and sgpbsrn1duttC1.c1), were all available. In 2001, the diffuse shortwave (SW) instruments were switched to shaded black and white instruments, and the name BSRN was switched to broadband radiometer station (BRS). Before that time, this VAP uses corrected diffuse SW from the DiffCorr1Dutt VAP as

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101

Initial Evaluation of the Cumulus Potential Scheme at the ACRF SGP Site  

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Meeting, Meeting, 12 March 2008 Initial Evaluation of the Cumulus Potential Scheme at the ACRF SGP Site Larry K. Berg, William I. Gustafson Jr., and Evgueni I. Kassianov Pacific Northwest National Laboratory ARM Science Team Meeting, 12 March 2008 Where are We Going? Development Simulation Evaluation Observations ARM Science Team Meeting, 12 March 2008 Development: Coupling Clouds to the Convective Boundary Layer * Shallow cumuli are turbulently coupled to the planetary boundary layer 4 3 2 1 0 Height (km) 6 5 4 3 2 1 0 Distance (km) Simulation courtesy of M. Ovtchinnikov ARM Science Team Meeting, 12 March 2008 Development: Coupling Clouds to the Convective Boundary Layer * Parameterization should represent this coupling * The Cumulus Potential (CuP) scheme is one way - Accounts for sub-grid

102

Anvil characteristics as seen by C-POL during the Tropical Warm Pool International Cloud Experiment (TWP-ICE)  

E-Print Network (OSTI)

The Tropical Pacific Warm Pool International Cloud Experiment (TWP-ICE) took place in Darwin, Australia in early 2006. C-band radar data from this experiment were used to characterize tropical anvil areal coverage, height, and thickness during the month-long field campaign. The morphology, evolution, and longevity of the anvil were analyzed as well as the relationship of the anvil to the rest of the precipitating system. In addition, idealized in-cloud radiative heating profiles were created based on the anvil observations. The anvil was separated into mixed (i.e., echo base below 6 km) and ice only categories. The experiment areal average coverage for both types of anvil was between 4-5% of the radar grid. Ice anvil thickness averaged 2.8 km and mixed anvil thickness averaged 6.7 km. No consistent diurnal signal was seen in the anvil, implying that the life cycle of the parent convection was of first order importance in determining the anvil height, thickness, and area. Areal peaks show that mixed anvil typically formed out of the stratiform region. Peak production in ice anvil usually followed the mixed anvil peak by 1-3 hr. Anvil typically lasted 4-10 hr after the initial convective rain area peak. The TWP-ICE experienced three distinct regimes: the active monsoon, dry monsoon, and break periods. During the entire experiment (except the active monsoon period) there was a strong negative correlation between ice anvil thickness and ice anvil height, a strong positive correlation between ice anvil area and thickness, and a greater variance in ice anvil bottom than ice anvil top. Anvil produced during the active regime had the most dramatic in-cloud radiative response with a maximum cooling of 0.45?° K day-1 at 12 km, a maximum heating of 3?° K day-1 at 9 km, and a secondary maximum heating of 1.2?° K day-1 at 5 km.

Frederick, Kaycee Loretta

2006-12-01T23:59:59.000Z

103

Evaluation of Cloud-Resolving Model Intercomparison Simulations Using TWP-ICE Observations: Precipitation and Cloud Structure  

SciTech Connect

The Tropical Warm Pool International Cloud Experiment (TWP-ICE) provided high quality model forcing and observational datasets through which detailed model and observational intercomparisons could be performed. In this first of a two part study, precipitation and cloud structures within nine cloud-resolving model simulations are compared with scanning radar reflectivity and satellite infrared brightness temperature observations during an active monsoon period from 19 to 25 January 2006. Most simulations slightly overestimate volumetric convective rainfall. Overestimation of simulated convective area by 50% or more in several simulations is somewhat offset by underestimation of mean convective rain rates. Stratiform volumetric rainfall is underestimated by 13% to 53% despite overestimation of stratiform area by up to 65% because stratiform rain rates in every simulation are much lower than observed. Although simulations match the peaked convective radar reflectivity distribution at low levels, they do not reproduce the peaked distributions observed above the melting level. Simulated radar reflectivity aloft in convective regions is too high in most simulations. In stratiform regions, there is a large spread in model results with none resembling observed distributions. Above the melting level, observed radar reflectivity decreases more gradually with height than simulated radar reflectivity. A few simulations produce unrealistically uniform and cold 10.8-?m infrared brightness temperatures, but several simulations produce distributions close to observed. Assumed ice particle size distributions appear to play a larger role than ice water contents in producing incorrect simulated radar reflectivity distributions aloft despite substantial differences in mean graupel and snow water contents across models.

Varble, Adam; Fridlind, Ann; Zipser, Edward J.; Ackerman, Andrew; Chaboureau, Jean-Pierre; Fan, Jiwen; Hill, Adrian; McFarlane, Sally A.; Pinty, Jean-Pierre; Shipway, Ben

2011-10-04T23:59:59.000Z

104

ARM - Publications: Science Team Meeting Documents  

NLE Websites -- All DOE Office Websites (Extended Search)

An Improved Technique for Producing MPL Backscatter Profiles Properly An Improved Technique for Producing MPL Backscatter Profiles Properly Characterized at All Ranges Flynn, C.J. and Powell, D.M., Pacific Northwest National Laboratory Eleventh Atmospheric Radiation Measurement (ARM) Science Team Meeting An important part of ARM's mission is the quantitative study of the effect of clouds and aerosol on radiative transfer and the energy budget. Micropulse Lidar (MPL) are an integral component of the ARM Program's measurement strategy with one deployed at each of the four major sites (SGP, TWP1, TWP2, and NSA). The MPL system is capable of producing vertical profiles of cloud and aerosol from ground level to the top of the atmosphere. However, the legitimacy of these profiles is sensitive to the calibration and system corrections of the individual MPL. In particular,

105

Surface Spectral Albedo Intensive Operational Period at the ARM SGP Site in august 2002: Results, Analysis, and Future Plans  

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Spectral Albedo Intensive Operational Period Spectral Albedo Intensive Operational Period at the ARM SGP Site in August 2002: Results, Analysis, and Future Plans A. P. Trishchenko and Y. Luo Canada Centre for Remote Sensing Ottawa, Ontario, Canada M. C. Cribb and Z. Li University of Maryland College Park, Maryland K. Hamm University of Oklahoma Norman, Oklahoma Introduction A surface spectral albedo Intensive Operational Period (IOP) at the Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) site was conducted during August 14-19, 2002, to meet the ARM Program need in a detailed knowledge of surface boundary conditions for atmospheric radiation studies. We measured surface spectral albedos/reflectances for several representative surface types and made a survey of landcover types over an area of approximately 10 km x 10 km centered

106

Towards Development of a Synthesized Database of Spatial and Temporal Surface Spectral Reflectivity Over the ARM SGP CART Area  

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Towards Development of a Synthesized Database of Towards Development of a Synthesized Database of Spatial and Temporal Surface Spectral Reflectivity Over the ARM SGP CART Area A. P. Trishchenko, Y. Luo, R. Latifovic, W. Park, J. Cihlar, and B. Hwang Canada Centre for Remote Sensing Ottawa, Ontario, Canada Z. Li and M. C. Cribb University of Maryland, College Park, Maryland Introduction Surface albedo is a key variable determining the disposition of solar radiation between the surface and the atmosphere. Reliable mapping of surface albedo and improved understanding of radiation interactions at the surface are required for advancing weather forecasting and climate studies. The ground-based observations are limited to a handful of locations sparsely distributed in the South Great Plains (SGP). Frequently, they represent only small-scale features of surface reflective properties and

107

Remotely Controlled, Continuous Observations of Infrared Radiance with the CSIRO/ARM Mark II Radiometer at the SGP CART Site  

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Remotely Controlled, Continuous Observations of Remotely Controlled, Continuous Observations of Infrared Radiance with the CSIRO/ARM Mark II Radiometer at the SGP CART Site C. M. R. Platt and R. T. Austin Department of Atmospheric Science Colorado State University Fort Collins, Colorado C. M. R. Platt and J. A. Bennett Commonwealth Scientific and Industrial Research Organization Atmospheric Research Aspendale, Victoria, Australia Abstract The Commonwealth Scientific and Industrial Research Organization/Atmospheric Radiation Measurement (CSIRO/ARM) Program Mark II infrared (IR) filter radiometer operated continuously at the Southern Great Plains (SGP) Cloud and Radiation Testbed (CART) site for a period of five weeks. Data of high quality were obtained by remote operation and data transfer with no evidence of spurious

108

Diurnal Cycle of Convection at the ARM SGP Site: Role of Large-Scale Forcing, Surface Fluxes, and Convective Inhibition  

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Diurnal Cycle of Convection at the ARM SGP Site: Diurnal Cycle of Convection at the ARM SGP Site: Role of Large-Scale Forcing, Surface Fluxes, and Convective Inhibition G. J. Zhang Center for Atmospheric Sciences Scripps Institution of Oceanography La Jolla, California Introduction Atmospheric convection undergoes strong diurnal variation over both land and oceans (Gray and Jacobson 1977; Dai 2001; Nesbitt and Zipser 2003). Because of the nature of the diurnal variation of solar radiation, the phasing of convection with solar radiation has a significant impact on the atmospheric radiation budget and cloud radiative forcing. A number of studies have investigated the possible mechanisms of the diurnal variation of convection (Gray and Jacobson 1977; Randall et al. 1991; Dai et al. 1999; Dai 2001). Yet, in regional and global climate models, the diurnal variation of

109

Evaluation of Cloud-Resolving Model Intercomparison Simulations Using TWP-ICE Observations: Precipitation and Cloud Structure  

SciTech Connect

The Tropical Warm Pool - International Cloud Experiment (TWP-ICE) provided high quality model forcing and observational datasets through which detailed model and observational intercomparisons could be performed. In this first of a two part study, precipitation and cloud structures within nine cloud-resolving model simulations are compared with scanning radar reflectivity and satellite infrared brightness temperature observations during an active monsoon period from 19 to 25 January 2006. Most simulations slightly overestimate volumetric convective rainfall. Overestimation of simulated convective area by 50% or more in several simulations is somewhat offset by underestimation of mean convective rain rates. Stratiform volumetric rainfall is underestimated by 13% to 53% despite overestimation of stratiform area by up to 65% because stratiform rain rates in every simulation are much lower than observed. Although simulations match the peaked convective radar reflectivity distribution at low levels, they do not reproduce the peaked distributions observed above the melting level. Simulated radar reflectivity aloft in convective regions is too high in most simulations. 29 In stratiform regions, there is a large spread in model results with none resembling 30 observed distributions. Above the melting level, observed radar reflectivity decreases 31 more gradually with height than simulated radar reflectivity. A few simulations produce 32 unrealistically uniform and cold 10.8-?m infrared brightness temperatures, but several 33 simulations produce distributions close to observed. Assumed ice particle size 34 distributions appear to play a larger role than ice water contents in producing incorrect 35 simulated radar reflectivity distributions aloft despite substantial differences in mean 36 graupel and snow water contents across models. 37

Varble, Adam C.; Fridlind, Ann; Zipser, Ed; Ackerman, Andrew; Chaboureau, Jean-Pierre; Fan, Jiwen; Hill, Adrian; McFarlane, Sally A.; Pinty, Jean-Pierre; Shipway, Ben

2011-06-24T23:59:59.000Z

110

Comparison of the CALIPSO satellite and ground-based observations of cirrus clouds at the ARM TWP sites  

SciTech Connect

Statistics of ice cloud macrophysical and optical properties from the Cloud-Aerosol LIdar with Orthogonal Polarization (CALIOP) instrument on board the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) satellite are compared with those from ground-based lidar observations over a 31 month period. Ground-based lidar observations are taken from the micropulse lidars (MPL) at the three Department of Energy Atmospheric Radiation Measurement (ARM) tropical western pacific (TWP) sites: Manus, Nauru and Darwin. CALIPSO observations show a larger cloud fraction at high altitudes while the ground-based MPLs show a larger cloud fraction at low altitudes. The difference in mean ice cloud top and base heights at the Manus and Nauru sites are all within 0.51 km, although differences are statistically significant. Mean ice cloud geometrical thickness agree to within 0.05 km at the Manus and Nauru sites. Larger differences exist at Darwin due to excessive degradation of the MPL output power during our sampling period. Both sets of observations show thicker clouds during the nighttime which may be real but could also be partially an artifact of the decreased signal-to-noise ratio during the daytime. The number of ice cloud layers per profile are also shown to be consistent after accounting for the difference in spatial resolution. For cloud optical depths, four different retrieval methods are compared, two for each set of observations. All products show that the majority of ice cloud optical depths ({approx}60%) fall below an optical depth of 0.2. For most comparisons all four retrievals agree to within the uncertainty intervals. We find that both CALIPSO retrievals agree best to ground-based optical depths when the lidar ratio in the latter is retrieved instead of set to a fixed value. Also thoroughly compared is the cloud properties for the subset of ice clouds which reside in the tropical tropopause layer (TTL).

Thorsen, Tyler J.; Fu, Q.; Comstock, Jennifer M.

2011-11-10T23:59:59.000Z

111

FINAL REPORT (DE-FG02-97ER62338): Single-column modeling, GCM parameterizations, and ARM data  

SciTech Connect

Our overall goal is the development of new and improved parameterizations of cloud-radiation effects and related processes, using ARM data at all three ARM sites, and the implementation and testing of these parameterizations in global models. To test recently developed prognostic parameterizations based on detailed cloud microphysics, we have compared SCM (single-column model) output with ARM observations at the SGP, NSA and TWP sites. We focus on the predicted cloud amounts and on a suite of radiative quantities strongly dependent on clouds, such as downwelling surface shortwave radiation. Our results demonstrate the superiority of parameterizations based on comprehensive treatments of cloud microphysics and cloud-radiative interactions. At the SGP and NSA sites, the SCM results simulate the ARM measurements well and are demonstrably more realistic than typical parameterizations found in conventional operational forecasting models. At the TWP site, the model performance depends strongly on details of the scheme, and the results of our diagnostic tests suggest ways to develop improved parameterizations better suited to simulating cloud-radiation interactions in the tropics generally. These advances have made it possible to take the next step and build on this progress, by incorporating our parameterization schemes in state-of-the-art three-dimensional atmospheric models, and diagnosing and evaluating the results using independent data. Because the improved cloud-radiation results have been obtained largely via implementing detailed and physically comprehensive cloud microphysics, we anticipate that improved predictions of hydrologic cycle components, and hence of precipitation, may also be achievable.

Richard C. J. Somerville

2009-02-27T23:59:59.000Z

112

Heterogeneous surface fluxes and their effects on the SGP CART site  

SciTech Connect

The treatment of subgrid-scale variations of surface properties and the resultant spatial variations of sensible and latent heat fluxes has received increasing attention in recent years. Mesoscale numerical simulations of highly idealized conditions, in which strong flux contrasts exist between adjacent surfaces, have shown that under some circumstances the secondary circulations induced by land-use differences can significantly affect the properties of the planetary boundary layer (PBL) and the region of the atmosphere above the PBL. At the Southern Great Plains (SGP) Cloud and Radiation Testbed (CART) site, the fluxes from different land-surface types are not expected to differ as dramatically as those found in idealized simulations. Although the corresponding effects on the atmosphere should thus be less dramatic, they are still potentially important. From an ARM perspective, in tests of single column models (SCMs) it would be useful to understand the effects of the lower boundary conditions on model performance. We describe here our initial efforts to characterize the variable surface fluxes over the CART site and to assess their effects on the PBL that are important for the performance of SCMs.

Doran, J.C.; Hu, Q.; Hubbe, J.M.; Liljegren, J.C.; Shaw, W.J.; Zhong, S. [Pacific Northwest Lab., Richland, WA (United States); Collatz, G.J. [Goddard Space Flight Center/NASA, Greenbelt, MD (United States)

1995-03-01T23:59:59.000Z

113

ARM - Publications: Science Team Meeting Documents  

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Improved Methods for Broadband Outdoor Radiometer Calibration (BORCAL) Improved Methods for Broadband Outdoor Radiometer Calibration (BORCAL) Wilcox, S.M., Andreas, A.M., Reda, I., and Myers, D.R., National Renewable Energy Laboratory Twelfth Atmospheric Radiation Measurement (ARM) Science Team Meeting The ARM Program deploys approximately 100 radiometers to measure broadband solar radiation at stations in the North Slope of Alaska (NSA), Southern Great Plains (SGP), and Tropical Western Pacific (TWP) Cloud and Radiation Testbed (CART) sites. Two calibration events performed at the SGP Radiometer Calibration Facility (RCF) each year maintain radiometer calibration traceability to the World Radiometric Reference and assure reliable and uniform measurements at each CART site. Calibrations are performed using the Radiometer Calibration and Characterization (RCC)

114

Tamás Várnai  

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of simulated 2-D solar radiative effects of simulated 2-D solar radiative effects over three ARM sites Tamás Várnai 1 and Jerry Y. Harrington 2 1 UMBC JCET and NASA GSFC, 2 Penn State University Project overview Dataset and flux results Nadir reflectance results (relevant to satellite remote sensing) Current dataset 1 year at NSA, SGP, TWP Microbase: cloud profiles (LWC, IWC, r e liq , r e ice ) Mergesonde: wind aloft (time diff. distance) Cloud classification at SGP Simulated 1-D & 2-D fluxes and nadir reflectances at 0.86 µm 0 20 40 60 80 100 -20 -15 -10 -5 0 5 10 15 20 Cumulative histogram value (%) Relative flux difference (%) (2D - 1D) / 1D Albedo Transmittance In-cloud actinic flux Solar zenith angle (Θ 0 ) dependence of 3D effects for various cloud types -15 -10

115

1  

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Multi-Filter Rotating Shadowband Radiometers Mentor Multi-Filter Rotating Shadowband Radiometers Mentor Report and Baseline Surface Radiation Network Submission Status G. Hodges Cooperative Institute for Research in Environmental Sciences University of Colorado Boulder, Colorado Overview Currently 24 multi-filter rotating shadowband radiometers (MFRSRs) operate within the Atmospheric Radiation Measurement (ARM) Program. Eighteen MFRSRs are located at Southern Great Plains (SGP) site, one is located at each of the North Slope of Alaska (NSA) and Tropical Western Pacific (TWP) sites, and one is part of the instrumentation of the ARM Mobile Facility. The SGP site, that has four extended facilities that are equipped for an MFRSR but do not have one due to instrument failure or a lack of spare instruments. Table 1 lists all the sites supporting MFRSRs along with the instrument

116

Cloud properties derived from two lidars over the ARM SGP site  

Science Conference Proceedings (OSTI)

[1] Active remote sensors such as lidars or radars can be used with other data to quantify the cloud properties at regional scale and at global scale (Dupont et al., 2009). Relative to radar, lidar remote sensing is sensitive to very thin and high clouds but has a significant limitation due to signal attenuation in the ability to precisely quantify the properties of clouds with a 20 cloud optical thickness larger than 3. In this study, 10-years of backscatter lidar signal data are analysed by a unique algorithm called STRucture of ATmosphere (STRAT, Morille et al., 2007). We apply the STRAT algorithm to data from both the collocated Micropulse lidar (MPL) and a Raman lidar (RL) at the Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) site between 1998 and 2009. Raw backscatter lidar signal is processed and 25 corrections for detector deadtime, afterpulse, and overlap are applied. (Campbell et al.) The cloud properties for all levels of clouds are derived and distributions of cloud base height (CBH), top height (CTH), physical cloud thickness (CT), and optical thickness (COT) from local statistics are compared. The goal of this study is (1) to establish a climatology of macrophysical and optical properties for all levels of clouds observed over the ARM SGP site 30 and (2) to estimate the discrepancies induced by the two remote sensing systems (pulse energy, sampling, resolution, etc.). Our first results tend to show that the MPLs, which are the primary ARM lidars, have a distinctly limited range where all of these cloud properties are detectable, especially cloud top and cloud thickness, but even actual cloud base especially during summer daytime period. According to the comparisons between RL and MPL, almost 50% of situations show a signal to noise ratio too low (smaller than 3) for the MPL in order to detect clouds higher than 7km during daytime period in summer. Consequently, the MPLderived annual cycle of cirrus cloud base (top) altitude is biased low, especially for daylight periods, compared with those derived from the RL data, which detects 5 cloud base ranging from 7.5 km in winter to 9.5 km in summer (and tops ranging from 8.6 to 10.5 km). The optically thickest cirrus clouds (COT>0.3) reach 50% of the total population for the Raman lidar and only 20% for the Micropulse lidar due to the difference of pulse energy and the effect of solar irradiance contamination. A complementary study using the cloud fraction 10 derived from the Micropulse lidar for clouds below 5 km and from the Raman lidar for cloud above 5 km allows for better estimation of the total cloud fraction between the ground and the top of the atmosphere. This study presents the diurnal cycle of cloud fraction for each season in comparisons with the Long et al. (2006) cloud fraction calculation derived from radiative flux analysis.

Dupont, Jean-Charles; Haeffelin, Martial; Morille, Y.; Comstock, Jennifer M.; Flynn, Connor J.; Long, Charles N.; Sivaraman, Chitra; Newsom, Rob K.

2011-02-16T23:59:59.000Z

117

Tropical Warm Pool International Cloud Experiment (TWP-ICE): Cloud and Rain Characteristics in the Australian Monsoon  

SciTech Connect

The impact of oceanic convection on its environment and the relationship between the characteristics of the convection and the resulting cirrus characteristics is still not understood. An intense airborne measurement campaign combined with an extensive network of ground-based observations is being planned for the region near Darwin, Northern Australia, during January-February, 2006, to address these questions. The Tropical Warm Pool International Cloud Experiment (TWP-ICE) will be the first field program in the tropics that attempts to describe the evolution of tropical convection, including the large scale heat, moisture, and momentum budgets, while at the same time obtaining detailed observations of cloud properties and the impact of the clouds on the environment. The emphasis will be on cirrus for the cloud properties component of the experiment. Cirrus clouds are ubiquitous in the tropics and have a large impact on their environment but the properties of these clouds are poorly understood. A crucial product from this experiment will be a dataset suitable to provide the forcing and testing required by cloud-resolving models and parameterizations in global climate models. This dataset will provide the necessary link between cloud properties and the models that are attempting to simulate them. The experiment is a collaboration between the U.S. Department of Energy (DOE) Atmospheric Radiation Measurement (ARM) Program, the Bureau of Meteorology (BoM), the National Aeronautics and Space Administration (NASA), the European Commission DG RTD-1.2, and several United States, Australian, Canadian, and European Universities. This experiment will be undertaken over a 4-week period in early 2006. January and February corresponds to the wet phase of the Australia monsoon. This season has been selected because, despite Darwins coastal location, the convection that occurs over and near Darwin at this time is largely of maritime origin with a large fetch over water. Based on previous experiments, the convection appears typical of maritime convection with widespread convection that has complex organization, but is not as deep or as intense as continental or coastal convection. Therefore, it is expected that the convection and cloud characteristics will be representative of conditions typical for wide areas of the tropics.

PT May; C Jakob; JH Mather

2004-05-30T23:59:59.000Z

118

Improvements in Representations of Cloud Microphysics for BBHRP and Models using Data Collected during M-PACE and TWP-ICE  

SciTech Connect

In our research we proposed to use data collected during the 2004 Mixed-Phase Arctic Cloud Experiment (MPACE) and the 2006 Tropical Warm Pool International Cloud Experiment (TWP-ICE) to improve retrievals of ice and mixed-phase clouds, to improve our understanding of how cloud and radiative processes affect cloud life cycles, and to develop and test methods for using ARM data more effectively in model. In particular, we proposed to: 1) use MPACE in-situ data to determine how liquid water fraction and cloud ice and liquid effective radius (r{sub ei} and r{sub ew}) vary with temperature, normalized cloud altitude and other variables for Arctic mixed-phase clouds, and to use these data to evaluate the performance of model parameterization schemes and remote sensing retrieval algorithms; 2) calculate rei and size/shape distributions using TWP-ICE in-situ data, investigate their dependence on cirrus type (oceanic or continental anvils or cirrus not directly traced to convection), and develop and test representations for MICROBASE; 3) conduct fundamental research enhancing our understanding of cloud/radiative interactions, concentrating on effects of small crystals and particle shapes and sizes on radiation; and 4) improve representations of microphysical processes for models (fall-out, effective density, mean scattering properties, rei and rew) and provide them to ARM PIs. In the course of our research, we made substantial progress on all four goals.

Greg M. McFarquhar

2010-02-22T23:59:59.000Z

119

ARM - TWP Manus Site  

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personnel at TWPO, provide a 24-hour support for daily operations and instrument troubleshooting. Momote Airport from the air. Momote Airport from the air. Instruments Current...

120

TWP Manus Site  

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personnel at TWPO, provide a 24-hour support for daily operations and instrument troubleshooting. Momote Airport from the air. Momote Airport from the air. Instruments Current...

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121

Surface Di-directional Reflectance Properties Over the ARM SGP Area from Satellite Multi-Platform Observations  

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Bi-Directional Reflectance Properties Bi-Directional Reflectance Properties Over the ARM SGP Area from Satellite Multi-Platform Observations Y. Luo, A. P. Trishchenko, and R. Latifovic Canada Centre for Remote Sensing Natural Resources Canada Ottawa, Ontario, Canada Z. Li Earth System Science Interdisciplinary Center University of Maryland College Park, Maryland Introduction Surface albedo is an important parameter in atmospheric radiation research. Good knowledge of surface bi-directional reflectance distribution function (BRDF) is essential in order to obtain the hemispheric reflectance (albedo) using data from satellite systems, which only view the ground at particular angles. Linear kernel-driven BRDF models have been commonly used for simple operational implementation of

122

ARM - Program Documents  

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Cloud Experiment (TWP-ICE): Cloud and Rain Characteristics in the Australian Monsoon (PDF, 1.2MB) DOEERARM-0401 2004 SGP Cloud and Land Surface Interaction Campaign...

123

Satellite and Surface Data Synergy for Developing a 3D Cloud Structure and Properties Characterization Over the ARM SGP. S...  

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Satellite and Surface Data Synergy for Developing Satellite and Surface Data Synergy for Developing a 3D Cloud Structure and Properties Characterization Over the ARM SGP Site Stage 1: Cloud Amounts, Optical Depths, and Cloud Heights Reconciliation I. Genkova and C. N. Long Pacific Northwest National Laboratory Richland, Washington P. W. Heck Analytical Services & Materials, Inc. Hampton, Virginia P. Minnis National Aeronautics and Space Administration Langley Research Center Hampton, Virginia Introduction One of the primary Atmospheric Radiation Measurement (ARM) Program objectives is to obtain measurements applicable to the development of models for better understanding of radiative processes in the atmosphere. We address this goal by building a three-dimensional (3D) characterization of the

124

Asymmetry in the Diurnal Cycle of Atmospheric Downwelling Radiation at the ARM SGP CF Site Over 1995-2001 Period  

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Asymmetry in the Diurnal Cycle of Atmospheric Asymmetry in the Diurnal Cycle of Atmospheric Downwelling Radiation at the ARM SGP CF Site Over 1995-2001 Period A. P. Trishchenko Canada Centre for Remote Sensing Ottawa, Ontario, Canada Introduction The shape of the diurnal cycle of atmospheric downwelling radiation is an important climatic feature of cloud-radiation interactions and atmospheric properties. Adequate characterization of this diurnal cycle is critical for accurate determination of monthly and seasonal radiation budgets from a limited data sampling. This is especially important for establishing the optimal sampling and temporal interpolation schemes employed in satellite radiation budget missions, such as Earth Radiation Budget Experiment (ERBE), Scanner for Radiation Budget (ScaRaB), and Clouds and Earth's Radiant Energy System

125

New Visible to Broadband Shortwave Conversions for Deriving Albedos from GOES-8 Over the ARM-SGP  

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New Visible to Broadband Shortwave Conversions for New Visible to Broadband Shortwave Conversions for Deriving Albedos from GOES-8 Over the ARM-SGP V. Chakrapani, D. R. Doelling, and M. M. Khaiyer Analytical Services and Materials, Inc. Hampton, Virginia P. Minnis National Aeronautics and Space Administration Langley Research Center Hampton, Virginia Introduction The radiation budget at the top of the atmosphere (TOA) is a quantity of fundamental importance to the Atmospheric Radiation Measurement (ARM) Program. Thus, it is necessary to measure the radiation budget components, broadband shortwave (SW) albedo and outgoing longwave radiation, as accurately as possible. Measurement of TOA broadband albedos over the ARM surface sites has only been possible since the advent of Clouds and the Earth's Radiant Energy System (CERES; Wielicki et al.

126

Techniques and Methods Used to Determine the Aerosol Best Estimate Value-Added Product at SGP Central Facility  

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Determine the Aerosol Best Estimate Value-Added Product at SGP Central Facility C. Sivaraman, D. D. Turner, and C. J. Flynn Pacific Northwest National Laboratory Richland, Washington Objective Profiles of aerosol optical properties are needed for radiative closure exercises such as the broadband heating rate profile (BBHRP) project (Mlawer et al. 2002) and the Shortwave Quality Measurement Experiment (QME). Retrieving cloud microphysical properties using radiation measurements in the shortwave, such as the spectral retrieval technique described in Daniel et al. (2002), also require the optical properties of the aerosols so that they can be accounted for in the retrieval process. The objective of the aerosol best estimate (ABE) value-added procedure (VAP) is to provide profiles of

127

Month-Long 2D Cloud-Resolving Model Simulation and Resultant Statistics of Cloud Systems Over the ARM SGP  

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Month-Long 2D Cloud-Resolving Model Simulation Month-Long 2D Cloud-Resolving Model Simulation and Resultant Statistics of Cloud Systems Over the ARM SGP X. Wu Department of Geological and Atmospheric Sciences Iowa State University Ames, Iowa X.-Z. Liang Illinois State Water Survey University of Illinois Urbana-Champaign, Illinois Introduction The cloud-resolving model (CRM) has recently emerged as a useful tool to develop improved representations of convections, clouds, and cloud-radiation interactions in general circulation models (GCMs). In particular, the fine spatial resolution allows the CRM to more realistically represent the detailed structure of cloud systems, including cloud geometric and radiative properties. The CRM simulations thus provide unique and comprehensive datasets, based on which more realistic GCM

128

Comparison of improved Aura Tropospheric Emission Spectrometer (TES) CO{sub 2} with HIPPO and SGP aircraft profile measurements  

SciTech Connect

Comparisons are made between mid-tropospheric Tropospheric Emission Spectrometer (TES) carbon dioxide (CO{sub 2}) satellite measurements and ocean profiles from three Hiaper Pole-to-Pole Observations (HIPPO) campaigns and land aircraft profiles from the United States Southern Great Plains (SGP) Atmospheric Radiation Measurement (ARM) site over a 4-yr period. These comparisons are used to characterize the bias in the TES CO{sub 2} estimates and to assess whether calculated and actual uncertainties and sensitivities are consistent. The HIPPO dataset is one of the few datasets spanning the altitude range where TES CO{sub 2} estimates are sensitive, which is especially important for characterization of biases. We find that TES CO{sub 2} estimates capture the seasonal and latitudinal gradients observed by HIPPO CO{sub 2} measurements; actual errors range from 0.81.2 ppm, depending on the campaign, and are approximately 1.4 times larger than the predicted errors. The bias of TES versus HIPPO is within 0.85 ppm for each of the 3 campaigns; however several of the sub-tropical TES CO{sub 2} estimates are lower than expected based on the calculated errors. Comparisons of aircraft flask profiles, which are measured from the surface to 5 km, to TES CO{sub 2} at the SGP ARM site show good agreement with an overall bias of 0.1 ppm and rms of 1.0 ppm. We also find that the predicted sensitivity of the TES CO{sub 2} estimates is too high, which results from using a multi-step retrieval for CO{sub 2} and temperature. We find that the averaging kernel in the TES product corrected by a pressure-dependent factor accurately reflects the sensitivity of the TES CO{sub 2} product.

Kulawik, S. S.; Worden, J. R.; Wofsy, S. C.; Biraud, S. C.; Nassar, R.; Jones, D. B.A.; Olsen, E. T.; Osterman, G. B.

2012-02-01T23:59:59.000Z

129

Use of ARM/NSA Data to Validate and Improve the Remote Sensing Retrieval of Cloud and Surface Properties in the Arctic from AVHRR Data  

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ARM/NSA Data to Validate and Improve the ARM/NSA Data to Validate and Improve the Remote Sensing Retrieval of Cloud and Surface Properties in the Arctic from AVHRR Data X. Xiong QSS Group, Inc. National Oceanic and Atmospheric Administration National Environmental Satellite, Data, and Information Service Office of Research and Applications Camp Springs, Maryland R. Storvold and C. Marty Geophysical Institute University of Alaska Fairbanks, Alaska K. H. Stamnes Stevens Institute of Technology Hoboken, New Jersey B. D. Zak Sandia National Laboratories Albuquerque, New Mexico Introduction Clouds in the Arctic have an important impact on the radiative energy balance. However, the effects of clouds still constitute one of the largest uncertainties in the study of climate change. Because the surface

130

Measurement of Boundary-Layer Temperature Profiles by a Scanning 5-MM Radiometer During the 1999 Winter NSA/AAO Radiometer Exp  

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Boundary-Layer Temperature Profiles by Boundary-Layer Temperature Profiles by a Scanning 5-MM Radiometer During the 1999 Winter NSA/AAO Radiometer Experiment and WVIOP 2000 V. Y. Leuski and E. R. Westwater Cooperative Institute for Research in the Environmental Sciences National Oceanic and Atmospheric Administration Environmental Technology Laboratory University of Colorado Boulder, Colorado Introduction A scanning 5-mm-wavelength radiometer was deployed during two Intensive Operational Periods (IOPs) at the Atmospheric Radiation Measurement (ARM) Program's Cloud and Radiation Testbed (CART) facilities. The first was conducted at the North Slope of Alaska (NSA) and Adjacent arctic Ocean (AAO) site near Barrow, Alaska, during March 1999. One goal was to evaluate the ability of an

131

1  

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Wave Cloud Radar Upgrades: Wave Cloud Radar Upgrades: Review, Status, and Plans K.B. Widener Pacific Northwest National Laboratory Richland, Washington K.P. Moran National Oceanic and Atmospheric Administration- Earth System Research Laboratory-Physical Sciences Division Boulder, Colorado Introduction The Atmospheric Radiation Measurement (ARM) Program currently operates five millimeter-wave cloud radars (MMCRs) at the ARM Climate Research Facility (ACRF) Southern Great Plains (SGP) site, North Slope of Alaska (NSA) locale's Barrow site, and Tropical Western Pacific (TWP) locale's Manus, Nauru, and Darwin sites. Currently, three different signal processors are deployed, and we are in process of upgrading the remaining two radars to provide higher reliability and efficiency along with

132

ARM - Publications: Science Team Meeting Documents  

NLE Websites -- All DOE Office Websites (Extended Search)

Improved Retrieval Of Cloud Liquid Water Path For ARM Microwave Improved Retrieval Of Cloud Liquid Water Path For ARM Microwave Radiometers Liljegren, J.C., Ames Laboratory Eighth Atmospheric Radiation Measurement (ARM) Science Team Meeting The Atmospheric Radiation Measurement (ARM) Program has deployed dual-frequency microwave water radiometers (MWRs) at its Cloud and Radiation Testbed (CART) sites in the U. S. Southern Great Plains (SGP), the Tropical Western Pacific (TWP), and the North Slope of Alaska/Adjacent Arctic Ocean (NSA/AAO). Although the integrated water vapor amount provided by these instruments has enjoyed increasing application, the primary purpose of these instruments has been to provide measurements of the integrated liquid water path in clouds. The liquid water path measurements have been widely used by ARM investigators to test cloud life cycle

133

ARM - Evaluation Product - CMWG Data - SCM-Forcing Data, Cloud  

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ProductsCMWG Data - SCM-Forcing Data, Cloud ProductsCMWG Data - SCM-Forcing Data, Cloud Microphysical Properties and Radiative Heating Profiles Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Evaluation Product : CMWG Data - SCM-Forcing Data, Cloud Microphysical Properties and Radiative Heating Profiles Site(s) GAN HFE NSA SGP TWP General Description SCM-forcing data are derived from the ARM Program observational data using the constrained variational analysis approach (Zhang and Lin 1997 and Zhang et al. 2001). The resulting products include both the large-scale forcing terms and the evaluation fields, which can be used for driving the Single-Column Models (SCMs) and Cloud Resolving Models (CRMs) and validating model simulations. Results from our studies are then used to

134

Sensitivity of Radiative Fluxes and Heating Rates to Cloud Microphysics  

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Sensitivity of Radiative Fluxes and Heating Sensitivity of Radiative Fluxes and Heating Rates to Cloud Microphysics S. F. Iacobellis and R. C. J. Somerville Scripps Institution of Oceanography University of California, San Diego La Jolla, California G. M. McFarquhar University of Illinois at Urbana-Champaign Urbana, Illinois D. L. Mitchell Desert Research Institute Reno, Nevada Introduction A single-column model (SCM) is used to examine the sensitivity of basic quantities such as atmospheric radiative heating rates and surface and top of atmosphere (TOA) radiative fluxes to various parameter- izations of clouds and cloud microphysics. The SCM was run at the Atmospheric Radiation Measurement (ARM) Program's Southern Great Plains (SGP), Tropical Western Pacific (TWP), and North Slope of Alaska (NSA) sites using forcing data derived from forecast products. The forecast

135

ARM - Evaluation Product - Sonde-Adjust  

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ProductsSonde-Adjust ProductsSonde-Adjust Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Evaluation Product : Sonde-Adjust Site(s) FKB GRW HFE NIM NSA PYE SGP TWP General Description The sonde-adjust VAP produces data that corrects documented biases in radiosonde humidity measurements. Unique fields contained within this datastream include smoothed original relative humidity, dry bias corrected relative humidity, and final corrected relative humidity. The smoothed RH field refines the relative humidity from integers - the resolution of the instrument - to fractions of a percent. This profile is then used to calculate the dry bias corrected field. The final correction fixes a time-lag problem and uses the dry-bias field as input into the algorithm.

136

How is the Data Quality Office Doing?  

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How is the Data Quality Office Doing? How is the Data Quality Office Doing? K. L. Sonntag, R. A. Peppler, A. R. Dean, and C. M. Shafer Cooperative Institute for Mesoscale Meteorological Studies University of Oklahoma Norman, Oklahoma Introduction The Atmospheric Radiation Measurement (ARM) Program has collected data from its Southern Great Plains (SGP) climate research facility since late 1992, from its Tropical Western Pacific (TWP) site since 1996, and from its North Slope of Alaska (NSA) site since 1997. There are numerous instrument platforms at each site, including radiometer suites that measure solar and terrestrial radiation; tower- mounted instruments that measure wind, temperature, and humidity; subterranean sensors that measure soil moisture and thermal properties; a host of cloud-observing instruments that measure cloud extent

137

Research Highlight  

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Micropulse Lidar-Derived Aerosol Optical Depth Climatology at ARM Sites Micropulse Lidar-Derived Aerosol Optical Depth Climatology at ARM Sites Worldwide Download a printable PDF Submitter: Kafle, D. N., University of California, Riverside Coulter, R. L., Argonne National Laboratory Area of Research: Aerosol Properties Working Group(s): Aerosol Life Cycle Journal Reference: Kafle DN and RL Coulter. 2013. "Micropulse lidar-derived aerosol optical depth climatology at ARM sites worldwide." Journal of Geophysical Research - Atmospheres, 118(13), 10.1002/jgrd.50536. Vertical profiles of multi-year annually averaged AOD (z) at different ARM sites: SGP, NSA, TWP, GRW, and FKB. Inset plots are the profiles of corresponding relative standard deviation, Srel (z). The corresponding 1-sigma measurement errors are given in horizontal bars.

138

liljegren-98.pdf  

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Improved Retrieval of Cloud Liquid Water Path Improved Retrieval of Cloud Liquid Water Path J. C. Liljegren Ames Laboratory Ames, Iowa Introduction The Atmospheric Radiation Measurement (ARM) Program has deployed dual-frequency microwave water radiometers (MWRs) (Liljegren 1994) at its Cloud and Radiation Testbed (CART) sites in the U. S. Southern Great Plains (SGP), the Tropical Western Pacific (TWP), and the North Slope of Alaska/Adjacent Arctic Ocean (NSA/AAO). Although the integrated water vapor amount provided by these instruments has enjoyed increasing application, the primary purpose of these instruments has been to provide measurements of the integrated liquid water path (LWP) in clouds. Although the LWP measurements have been widely used by ARM investigators, shortcomings in the present statistical

139

ARM - Submitting Proposals : Guidelines  

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govField CampaignsSubmitting Proposals : Guidelines govField CampaignsSubmitting Proposals : Guidelines Schedule and Availability Preproposals now open for AMF and AAF Preproposals due 1 Feb Invited full proposals due 1 May AAF available Dec 2015 AMF1 available Apr 2016 AMF2 available early 2017 AMF3 available for guest instrumentation or intensive operational periods Forms Propose a Campaign Form Instrument Support Request (ISR) Form (Word, 89KB) Documentation Steps to Send Campaign Data to ARM Data Archive Field Campaign Guidelines (PDF, 1.1MB) Submitting Proposals : Guidelines Proposals are welcome from all members of the scientific community for conducting field campaigns and scientific research using the ARM Climate Research Facility sites at the Southern Great Plains (SGP), North Slope of Alaska (NSA), Tropical Western Pacific (TWP), one of the ARM Mobile

140

ARM - PI Product - Atmospheric State, Cloud Microphysics & Radiative Flux  

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ProductsAtmospheric State, Cloud Microphysics & ProductsAtmospheric State, Cloud Microphysics & Radiative Flux Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send PI Product : Atmospheric State, Cloud Microphysics & Radiative Flux 1997.01.01 - 2010.12.31 Site(s) NSA SGP TWP General Description This data product contains atmospheric thermodynamics, cloud properties, radiative fluxes and radiative heating rates. The data represent a characterization of the physical state of the atmospheric column compiled on a five-minute temporal and 90m vertical grid. Sources for this information include raw measurements, cloud property and radiative retrievals, retrievals and derived variables from other third-party sources, and radiative calculations using the derived quantities.

Note: This page contains sample records for the topic "nsa sgp twp" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


141

ARM - Instrument - avhrr  

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govInstrumentsavhrr govInstrumentsavhrr Documentation AVHRR : XDC documentation ARM Data Discovery Browse Data Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Instrument : Advanced Very High Resolution Radiometer (AVHRR) Instrument Categories Satellite Observations General Overview Measurements from the Advanced Very High Resolution Radiometer (AVHRR) on the NOAA polar orbiting satellites taken over the NSA, SHB, SGP, and TWP sites are available for distribution to the ARM community. The files are in HDF. The AVHRR data from the Australian Bureau of Meteorology (BOM) Darwin site have not yet been converted to HDF. The raw data are in ASDA (Australian Satellite Data Archive) Format.. Output Datastreams avhrr10 : AVHRR: albedo and brightness temp., NOAA-10 Satellite

142

ARM - Data Quality Program  

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Quality Program Quality Program DQ Resources Data Quality Assessment and Control Report (PDF, 747KB) Data Quality Office Data Quality Problem Reporting (DQPR) Contact Us Submit Data Quality Findings Randy Peppler, Data Quality Manager Ken Kehoe, Data Quality Specialist Justin Monroe, Data Quality Specialist Adam Theisen, Data Quality Specialist Sean Moore, Data Quality Consultant Instrument and Site Contacts Instrument Mentors AAF Contacts AMF Contacts NSA Site Contacts SGP Site Contacts TWP Site Contacts Data Quality Program Introduction One of the goals of the ARM Climate Research Facility is to provide datastreams of quality suitable for scientific research. Maintaining data quality for an organization program of the size and complexity of the ARM Facility is a significant challenge; efforts toward this end have matured

143

ARM - PI Product - Direct Aerosol Forcing Uncertainty  

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ProductsDirect Aerosol Forcing Uncertainty ProductsDirect Aerosol Forcing Uncertainty Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send PI Product : Direct Aerosol Forcing Uncertainty Site(s) NSA SGP TWP General Description Understanding sources of uncertainty in aerosol direct radiative forcing (DRF), the difference in a given radiative flux component with and without aerosol, is essential to quantifying changes in Earth's radiation budget. We examine the uncertainty in DRF due to measurement uncertainty in the quantities on which it depends: aerosol optical depth, single scattering albedo, asymmetry parameter, solar geometry, and surface albedo. Direct radiative forcing at the top of the atmosphere and at the surface as well as sensitivities, the changes in DRF in response to unit changes in

144

ARM - Evaluation Product - Merged Sounding VAP  

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ProductsMerged Sounding VAP ProductsMerged Sounding VAP Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Evaluation Product : Merged Sounding VAP Site(s) FKB GRW HFE NIM NSA PYE SGP TWP General Description This value-added product (VAP) uses a combination of observations from radiosonde soundings, the microwave radiometer, surface meteorological instruments, and ECMWF model output with a sophisticated scaling/interpolation/smoothing scheme in order to define profiles of the atmospheric thermodynamic state. These profiles are calculated at one-minute time resolution and 266 vertical levels which vary such that greater detail (20 meters) is captured near the surface with the resolution becoming coarser (200 meters) as the maximum altitude - 20 km above mean

145

Scanning ARM Cloud Radar Handbook  

SciTech Connect

The scanning ARM cloud radar (SACR) is a polarimetric Doppler radar consisting of three different radar designs based on operating frequency. These are designated as follows: (1) X-band SACR (X-SACR); (2) Ka-band SACR (Ka-SACR); and (3) W-band SACR (W-SACR). There are two SACRs on a single pedestal at each site where SACRs are deployed. The selection of the operating frequencies at each deployed site is predominantly determined by atmospheric attenuation at the site. Because RF attenuation increases with atmospheric water vapor content, ARM's Tropical Western Pacific (TWP) sites use the X-/Ka-band frequency pair. The Southern Great Plains (SGP) and North Slope of Alaska (NSA) sites field the Ka-/W-band frequency pair. One ARM Mobile Facility (AMF1) has a Ka/W-SACR and the other (AMF2) has a X/Ka-SACR.

Widener, K; Bharadwaj, N; Johnson, K

2012-06-18T23:59:59.000Z

146

Microsoft Word - lesht.doc  

NLE Websites -- All DOE Office Websites (Extended Search)

Comparison of ECMWF Model Analyses with the Observed Comparison of ECMWF Model Analyses with the Observed Upper-Air Temperature and Relative Humidity Climatology at the ARM NSA, SGP, and TWP Climate Research Facility Sites B. M. Lesht and J. C. Lijlegren Argonne National Laboratory Argonne, Illinois L. M. Miloshevich National Center for Atmospheric Research Boulder, Colorado Introduction Analyses of output from the European Centre for Medium-range Weather Forecasting (ECMWF 1994) model often are used for evaluating both observations (Ovarlez and van Velthoven 1997, Comstock and Jakob 2004) and the output of other models and satellite retrievals (Soden and Bretherton 1994). Although radiosonde observations are assimilated into the model forecasts, data collected above 300 hPa are not used, primarily because radiosondes are considered inaccurate at low temperatures and water

147

ARM - NSA Contacts  

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UIC Science, LLC, Cell: 907.878.4780 Site Scientist - Johannes Verlinde, The Pennsylvania State University Rapid Response Team Manager - Martin Stuefer, University of Alaska,...

148

Measurement and Modeling of Vertically Resolved Aerosol Optical Properties and Radiative Fluxes Over the ARM SGP Site During the May 2003 Aerosol IOP  

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Measurement and Modeling Measurement and Modeling of Vertically Resolved Aerosol Optical Properties and Radiative Fluxes Over the ARM SGP Site During the May 2003 Aerosol IOP B. Schmid and J. Redemann Bay Area Environmental Research Institute National Aeronautics and Space Administration Ames Research Center Moffett Field, California W. P. Arnott Desert Research Institute Reno, Nevada A. Bucholtz and J. Reid Naval Research Laboratory Monterey, California P. Colarco Earth System Science Interdisciplinary Center University of Maryland College Park, Maryland D. Covert and R. Elleman University of Washington Seattle, Washington J. Eilers, P. Pilewskie, and A. Strawa National Aeronautics and Space Administration Ames, Research Center Moffett Field, California R. A. Ferrare

149

ARM - SGP Boundary Facility  

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facilities-located at Hillsboro, Kansas; Morris, Oklahoma; Purcelll, Oklahoma and Vici, Oklahoma (north, east, south and west, respectively)-marked the approximate midpoint of...

150

A Simulation Study of Shallow Moist Convection and Its Impact on the Atmospheric Boundary Layer  

Science Conference Proceedings (OSTI)

By comparing regional model simulations with the observations collected at the southern Great Plains (SGP) site and the tropical western Pacific (TWP) Nauru site of the Atmospheric Radiation Measurement (ARM) project, this paper evaluates the ...

Ping Zhu; Christopher S. Bretherton

2004-10-01T23:59:59.000Z

151

NSA-Old Aspen Site  

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aspen forest TE-6 does biomass and allometry readings Aspen trees from the OA canopy tower in spring. This picture is looking at the ground through the aspen trees from the top...

152

ARM - SGP Radiometric Calibration Facility  

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pyrgeometers. The ARM Climate Research Facility requires accurate measurements of solar radiation from radiometers used in ground-based networks and airborne instrument...

153

PowerPoint Presentation  

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24 LDR Dry Period 20061115 clutter lidar only radar radar+lidar clear no lidar Summer Monsoon 20060722 Site Dates Available NSA 1998.03.25 - 2006.09.27 SGP 1996.11.08 - 2006.08.09...

154

Sheridan-PJ  

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In Situ Measurement of Aerosol Light Absorption and Single-Scattering Albedo at the NSA and SGP CART Sites P. J. Sheridan, 1 D. J. Delene, and J. A. Ogren National Oceanic and...

155

ARM - TWP Darwin Site - Aussie Trivia  

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of Western Australia, is also the capital city in the world with the most consistent wind. The welcome breeze of the "Fremantle Doctor"' arrives to cool down beach goers...

156

ARM - Publications: Science Team Meeting Documents  

NLE Websites -- All DOE Office Websites (Extended Search)

Aerosol Indirect Effect: Evidence from the ARM SGP and NSA Sites Aerosol Indirect Effect: Evidence from the ARM SGP and NSA Sites Penner, J.E.(a), Chen, Y.(a), and Dong, X.(b), University of Michigan (a), University of North Dakota (b) Thirteenth Atmospheric Radiation Measurement (ARM) Science Team Meeting The ARM SGP site and the NSA site provide a unique opportunity to examine the effects of aerosols on cloud optical properties because the aerosol concnetrations at each site span the range between polluted and clean conditions. Here, we examine whether the effect of aerosols on clouds can adequately explain the observed relationship between the liquid water path observed at each site and the cloud optical depth required to determine the observed surface flux. Aerosol number concentration at the SGP site was determined from the observed CN number concentration as well as the

157

ARM - Field Campaign - NSA Snow IOP  

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Lead Scientist : Johannes Verlinde For data sets, see below. Description Measurement of ice-phase precipitation in the Arctic remains a challenge (e.g. Goodison et al. 1998,...

158

SGP-TR-32 STANFORD GEOTHERMAL PROGRAM  

E-Print Network (OSTI)

to estimate the number of adsorption layers, the BET cell shown in Fig. 4 has already been used to determine \\ % SAMPLE HOLDER SAS CYLINDER FIGURE 4, BET CELL USED TO DETERMINE ROCK SURFACE AREA 6 #12;.-c 0- c? a =' m by hydraulic fracturing by LASL in the hot, dry rock experiment in New Mexico. The results of this first 75-day

Stanford University

159

Tower Temperature and Humidity Sensors (TWR) Handbook  

Science Conference Proceedings (OSTI)

Three tall towers are installed at the Atmospheric Radiation Measurement (ARM) Climate Research Facility: a 60-meter triangular tower at the Southern Great Plains (SGP) Central Facility (CF), a 21-meter walkup scaffolding tower at the SGP Okmulgee forest site (E21), and a 40-meter triangular tower at the North Slope of Alaska (NSA) Barrow site. The towers are used for meteorological, radiological, and other measurements.

Cook, DR

2010-02-01T23:59:59.000Z

160

ARM's Atmospheric Emitted Radiance Interferometer (AERI) Data  

DOE Data Explorer (OSTI)

The atmospheric emitted radiance interferometer (AERI) measures the absolute infrared spectral radiance (watts per square meter per steradian per wavenumber) of the sky directly above the instrument. The spectral measurement range of the instrument is 3300 to 520 wavenumbers (cm-1) or 3-19.2 microns for the normal-range instruments and 3300 to 400 cm-1 or 3-25 microns for the extended-range polar instruments. Spectral resolution is 1.0 cm-1. Instrument field-of-view is 1.3 degrees. A calibrated sky radiance spectrum is produced every 8 minutes in normal mode and every minute in rapid sampling mode. The actual sample scan time is 20-30 sec in rapid sampling mode with periodic gaps when the instrument is looking at the blackbodies. Rapid sampling will become available in all AERIs. Rapid sampling time will eventually be reduced to data every 20 seconds. The AERI data can be used for (1) evaluating line-by-line radiative transport codes, (2) detecting/quantifying cloud effects on ground-based measurements of infrared spectral radiance (and hence is valuable for cloud property retrievals), and (3) calculating vertical atmospheric profiles of temperature and water vapor and the detection of trace gases.[Copied from http://www.arm.gov/instruments/aeri]

The ARM Archive at Oak Ridge National Laboratory holds data collected from the AERI for three of the permanent ARM sites, North Slope Alaska (NSA), Southern Great Plains (SGP), and the Tropical Western Pacific (TWP), as well as from mobile facilities used during specific field campaigns. AERI data has been collected since 1995.

Note: This page contains sample records for the topic "nsa sgp twp" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


161

Data systems for science integration within the Atmospheric Radiation Measurement Program  

SciTech Connect

The Atmospheric Radiation Measurement (ARM) Program was developed by the US Department of Energy to support the goals and mission of the US Global Change Research Program. The purpose of the ARM program is to improve the predictive capabilities of General Circulation Models (GCMs) in their treatment of clouds and radiative transfer effects. Three experimental testbeds were designed for the deployment of instruments to collect atmospheric data used to drive the GCMs. Each site, known as a Cloud and Radiation Testbed (CART), consists of a highly available, redundant data system for the collection of data from a variety of instrumentation. The first CART site was deployed in April 1992 in the Southern Great Plains (SGP), Lamont, Oklahoma, with the other two sites to follow in early 1996 in the Tropical Western Pacific (TWP) and in 1997 on the North Slope of Alaska (NSA). Approximately 1.5 GB of data are transferred per day via the Internet from the CART sites, and external data sources to the ARM Experiment Center (EC) at Pacific Northwest Laboratory in Richland, Washington. The Experimental Center is central to the ARM data path and provides for the collection, processing, analysis and delivery of ARM data. Data from the CART sites from a variety of instrumentation, observational systems and from external data sources are transferred to the Experiment Center. The EC processes these data streams on a continuous basis to provide derived data products to the ARM Science Team in near real-time while maintaining a three-month running archive of data.

Gracio, D.K.; Hatfield, L.D.; Yates, K.R.; Voyles, J.W. [Pacific Northwest Lab., Richland, WA (United States); Tichler, J.L. [Brookhaven National Lab., Upton, NY (United States); Cederwall, R.T.; Laufersweiler, M.J.; Leach, M.J. [Lawrence Livermore National Lab., CA (United States); Singley, P. [Oak Ridge National Lab., TN (United States)

1995-12-31T23:59:59.000Z

162

Initial results from ensemble SCM simulations of TWP-ICE  

NLE Websites -- All DOE Office Websites (Extended Search)

high cloud. The model high cloud is sensitive to the forcing during the suppressed monsoon. There is insufficient low-level cloud during the suppressed monsoon. LW Radiation...

163

ARM-UAV TWP-ICE Payload Instrumentation Details  

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Payload Instrumentation Details McCoy, Robert Sandia National Laboratories Tooman, Tim Sandia National Laboratories McFarquhar, Greg University of Illinois Category: Field...

164

MISR-Derived Statistics of Cumulus Geometry at TWP Site  

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statistics of the cumulus geometry are presented in Figure 5a and Table 1a. There is a weak positive relationship between fluctuations of cloud base and cloud top (correlation...

165

EVALUATING CLOUD RETRIEVAL ALGORITHMS WITH THE ARM BBHRP FRAMEWORK  

E-Print Network (OSTI)

of liquid, ice, and mixed-phase clouds have been processed in BBHRP for the ACRF Southern Great Plains (SGP, and phase of clouds above each ACRF site. Various approaches to retrieve the microphysical properties, including those from Microbase, the current `reference' retrieval approach in BBHRP. At the NSA, mixed-phase

166

Surface and Tower Meteorological Instrumentation at NSA Handbook - January 2006  

SciTech Connect

The Surface and Tower Meteorological Instrumentation at Atqasuk (METTWR2H) uses mainly conventional in situ sensors to measure wind speed, wind direction, air temperature, dew point and humidity mounted on a 10-m tower. It also obtains barometric pressure, visibility, and precipitation data from sensors at or near the base of the tower. In addition, a Chilled Mirror Hygrometer is located at 1 m for comparison purposes. Temperature and relative humidity probes are mounted at 2 m and 5 m on the tower. For more information, see the Surface and Tower Meteorological Instrumentation at Atqasuk Handbook.

MT Ritsche

2006-01-30T23:59:59.000Z

167

ARM/NSA ES&H Policy Statement  

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all who work at, use, or visit the ACRFNSAAAO Site. The Site's ES&H policies and procedures are designed to ensure a safe work environment for Sandia employees, Sandia...

168

ARM - Publications: Science Team Meeting Documents: The SGP Aerosol...  

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banner Cart Icon Cart | Home | People | Site Index Atmospheric Radiation Measurement Climate Research Facility US Department of Energy About Science Campaigns Sites Instruments...

169

Surface Albedo at ARM SGP from Helicopter Observations  

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model (Fu and Liou 1993), ARM profile information and aerosols, and albedo spectral shape from the CARE experiment. Surface albedo is then adjusted such that model fluxes...

170

Investigation of SGP Atmospheric Moisture Budget for CLASIC ?...  

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of a recently completed investigation of the moisture budget over the Midwestern Corn Belt (Zangvil et al. 2001, 2004) This study will be expanded with * Extended seasons...

171

sgp_stratus_poster_v1.0.ppt  

NLE Websites -- All DOE Office Websites (Extended Search)

overlaid on the LES profiles. *This stratus case was not accompanied by consistent subsidence and slowly varying advective forcings typical of a marine barotropic atmosphere....

172

An Improved Cloud Classification Algorithm Based on the SGP CART...  

NLE Websites -- All DOE Office Websites (Extended Search)

studies which need to group clouds according to cloud types, but also provides necessary information to implement different retrieval algorithms to generate integrated cloud...

173

A Comparison Between Modeled and Measured Clear-Sky Radiative Shortwave Fluxes in Arctic Environments, with Special Emphasis on Diffuse Radiation  

SciTech Connect

The ability of the SBDART radiative transfer model to predict clear-sky diffuse and direct normal broadband shortwave irradiances is investigated. Model calculations of these quantities are compared with data from the Atmospheric Radiation Measurement (ARM) programs Southern Great Plains (SGP) and North Slope of Alaska (NSA) sites. The model tends to consistently underestimate the direct normal irradiances at both sites by about 1%. In regards to clear-sky diffuse irradiance, the model overestimates this quantity at the SGP site in a manner similar to what has been observed in other studies (Halthore and Schwartz, 2000). The difference between the diffuse SBDART calculations and Halthore and Schwartzs MODTRAN calculations is very small, thus demonstrating that SBDART performs similarly to MODTRAN. SBDART is then applied to the NSA site, and here it is found that the discrepancy between the model calculations and corrected diffuse measurements (corrected for daytime offsets, Dutton et al., 2001) is 0.4 W/m2 when averaged over the 12 cases considered here. Two cases of diffuse measurements from a shaded black and white pyranometer are also compared with the calculations and the discrepancy is again minimal. Thus, it appears as if the diffuse discrepancy that exists at the SGP site does not exist at the NSA sites. We cannot yet explain why the model predicts diffuse radiation well at one site but not at the other.

Barnard, James C.; Flynn, Donna M.

2002-10-08T23:59:59.000Z

174

Parameterizing Size Distribution in Ice Clouds  

SciTech Connect

PARAMETERIZING SIZE DISTRIBUTIONS IN ICE CLOUDS David L. Mitchell and Daniel H. DeSlover ABSTRACT An outstanding problem that contributes considerable uncertainty to Global Climate Model (GCM) predictions of future climate is the characterization of ice particle sizes in cirrus clouds. Recent parameterizations of ice cloud effective diameter differ by a factor of three, which, for overcast conditions, often translate to changes in outgoing longwave radiation (OLR) of 55 W m-2 or more. Much of this uncertainty in cirrus particle sizes is related to the problem of ice particle shattering during in situ sampling of the ice particle size distribution (PSD). Ice particles often shatter into many smaller ice fragments upon collision with the rim of the probe inlet tube. These small ice artifacts are counted as real ice crystals, resulting in anomalously high concentrations of small ice crystals (D < 100 m) and underestimates of the mean and effective size of the PSD. Half of the cirrus cloud optical depth calculated from these in situ measurements can be due to this shattering phenomenon. Another challenge is the determination of ice and liquid water amounts in mixed phase clouds. Mixed phase clouds in the Arctic contain mostly liquid water, and the presence of ice is important for determining their lifecycle. Colder high clouds between -20 and -36 oC may also be mixed phase but in this case their condensate is mostly ice with low levels of liquid water. Rather than affecting their lifecycle, the presence of liquid dramatically affects the cloud optical properties, which affects cloud-climate feedback processes in GCMs. This project has made advancements in solving both of these problems. Regarding the first problem, PSD in ice clouds are uncertain due to the inability to reliably measure the concentrations of the smallest crystals (D < 100 m), known as the small mode. Rather than using in situ probe measurements aboard aircraft, we employed a treatment of ice cloud optical properties formulated in terms of PSD parameters in combination with remote measurements of thermal radiances to characterize the small mode. This is possible since the absorption efficiency (Qabs) of small mode crystals is larger at 12 m wavelength relative to 11 m wavelength due to the process of wave resonance or photon tunneling more active at 12 m. This makes the 12/11 m absorption optical depth ratio (or equivalently the 12/11 m Qabs ratio) a means for detecting the relative concentration of small ice particles in cirrus. Using this principle, this project tested and developed PSD schemes that can help characterize cirrus clouds at each of the three ARM sites: SGP, NSA and TWP. This was the main effort of this project. These PSD schemes and ice sedimentation velocities predicted from them have been used to test the new cirrus microphysics parameterization in the GCM known as the Community Climate Systems Model (CCSM) as part of an ongoing collaboration with NCAR. Regarding the second problem, we developed and did preliminary testing on a passive thermal method for retrieving the total water path (TWP) of Arctic mixed phase clouds where TWPs are often in the range of 20 to 130 g m-2 (difficult for microwave radiometers to accurately measure). We also developed a new radar method for retrieving the cloud ice water content (IWC), which can be vertically integrated to yield the ice water path (IWP). These techniques were combined to determine the IWP and liquid water path (LWP) in Arctic clouds, and hence the fraction of ice and liquid water. We have tested this approach using a case study from the ARM field campaign called M-PACE (Mixed-Phase Arctic Cloud Experiment). This research led to a new satellite remote sensing method that appears promising for detecting low levels of liquid water in high clouds typically between -20 and -36 oC. We hope to develop this method in future research.

DeSlover, Daniel; Mitchell, David L.

2009-09-25T23:59:59.000Z

175

ARM - Facility News Article  

NLE Websites -- All DOE Office Websites (Extended Search)

New Data Loggers Deployed New Data Loggers Deployed Bookmark and Share As shown in this partial screen capture, the Real Time Monitoring and Control feature displays data that allows local observers to quickly check the status of the instrument system. As shown in this partial screen capture, the Real Time Monitoring and Control feature displays data that allows local observers to quickly check the status of the instrument system. As part of ongoing effort to upgrade data loggers and logging systems throughout the ARM Climate Research Facility, new Campbell Loggers (version CR23X) are being installed at the Tropical Western Pacific (TWP) and at the North Slope of Alaska (NSA) locales. In fall 2003, Campbell Loggers for the surface meteorology systems at NSA were installed. In June 2004, Campbell

176

Vertical Velocity Statistics in Fair-Weather Cumuli at the ARM TWP Nauru Climate Research Facility  

Science Conference Proceedings (OSTI)

Fair-weather cumuli are fundamental in regulating the vertical structure of water vapor and entropy in the lowest 23 km of the earths atmosphere over vast areas of the oceans. In this study, a long record of profiling cloud radar observations ...

Pavlos Kollias; Bruce Albrecht

2010-12-01T23:59:59.000Z

177

Statistics of Storm Updraft Velocities from TWP-ICE Including Verification with Profiling Measurements  

Science Conference Proceedings (OSTI)

Comparisons between direct measurements and modeled values of vertical air motions in precipitating systems are complicated by differences in temporal and spatial scales. On one hand, vertically profiling radars more directly measure the vertical ...

Scott Collis; Alain Protat; Peter T. May; Christopher Williams

2013-08-01T23:59:59.000Z

178

ARM - Publications: Science Team Meeting Documents  

NLE Websites -- All DOE Office Websites (Extended Search)

A Continuous Baseline Microphysical Retrieval (MICROBASE): Status of SGP A Continuous Baseline Microphysical Retrieval (MICROBASE): Status of SGP Version 1.2 and Prototype TWP Version Miller, M.A.(a), Johnson, K.L.(a), Jensen, M.P.(b), Mace, G.G.(c), Dong, X.(d), and Vogelmann, A.M.(a), Brookhaven National Laboratory (a), Columbia University (b), University of Utah (c), University of North Dakota (d) Fourteenth Atmospheric Radiation Measurement (ARM) Science Team Meeting The interaction of clouds with incoming and outgoing radiation streams produces discontinuous regions of heating and cooling within the atmospheric column. These regions can influence the atmospheric circulations at multiple scales, as well as modify the existing cloud structures. The Broadband Heating Rate Project (BBHRP) within ARM has the goal of producing instantaneous snapshots of the heating and cooling rate

179

Slide 1  

NLE Websites -- All DOE Office Websites (Extended Search)

Radiative Processes Working Group: Radiative Processes Working Group: Value Added Product (VAP) Updates Sally McFarlane RPWG Translator RPWG Breakout March 23,2009 2 Status of RPWG Operational VAPs BE Flux (Best Estimate Flux from 3 radiometers at SGP) run daily up through current QC RAD (Data Quality Assessment for Radiation Data) c1, s1 level data -current at all sites c2 level data - processing global shortwave correction; waiting for information on instrument swap-outs c1, s1 level data in archive for AMF from Pt. Reyes and COPS Investigating tracker problem in Niamey data Will begin processing China data shortly Shortwave Flux Analysis Runs monthly on all fixed sites except Darwin (processed once/year) and NSA (not implemented); 1-2 months behind current Adding NSA data; code implemented, currently evaluating test cases

180

DISCLAIMER  

NLE Websites -- All DOE Office Websites (Extended Search)

050 050 Towers Handbook DR Cook February 2010 Work supported by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research February 2010, DOE/SC-ARM/TR-050 iii Acronyms and Abbreviations ARM Atmospheric Radiation Measurement Climate Research Facility CF Central Facility CO 2 FLX Carbon Dioxide Flux Measurement System DQ Data Quality ECOR Eddy Correlation System GPS global positioning system MFR Multi-Filter Radiometer NSA North Slope of Alaska PGS precision gas system PRTD Platinum Resistance Temperature Detector RMS root mean square SGP Southern Great Plains SIRS Solar and Infrared Station SMOS Surface Meteorological Observation Station Also, see the ARM Acronyms and Abbreviations.

Note: This page contains sample records for the topic "nsa sgp twp" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


181

Eddy Correlation Flux Measurement System (ECOR) Handbook  

SciTech Connect

The eddy correlation (ECOR) flux measurement system provides in situ, half-hour measurements of the surface turbulent fluxes of momentum, sensible heat, latent heat, and carbon dioxide (CO2) (and methane at one Southern Great Plains extended facility (SGP EF) and the North Slope of Alaska Central Facility (NSA CF). The fluxes are obtained with the eddy covariance technique, which involves correlation of the vertical wind component with the horizontal wind component, the air temperature, the water vapor density, and the CO2 concentration.

Cook, DR

2011-01-31T23:59:59.000Z

182

Evaluating Global Aerosol Models and Aerosol and Water Vapor Properties Near Clouds  

Science Conference Proceedings (OSTI)

Project goals: (1) Use the routine surface and airborne measurements at the ARM SGP site, and the routine surface measurements at the NSA site, to continue our evaluations of model aerosol simulations; (2) Determine the degree to which the Raman lidar measurements of water vapor and aerosol scattering and extinction can be used to remotely characterize the aerosol humidification factor; (3) Use the high temporal resolution CARL data to examine how aerosol properties vary near clouds; and (4) Use the high temporal resolution CARL and Atmospheric Emitted Radiance Interferometer (AERI) data to quantify entrainment in optically thin continental cumulus clouds.

Richard A. Ferrare; David D. Turner

2011-09-01T23:59:59.000Z

183

Atmospheric Radiation Measurement Program Climate Research Facility Operations Quarterly Report. October 1 - December 31, 2010.  

Science Conference Proceedings (OSTI)

Individual raw datastreams from instrumentation at the Atmospheric Radiation Measurement (ARM) Climate Research Facility fixed and mobile sites are collected and sent to the Data Management Facility (DMF) at Pacific Northwest National Laboratory (PNNL) for processing in near-real time. Raw and processed data are then sent approximately daily to the ARM Archive, where they are made available to users. For each instrument, we calculate the ratio of the actual number of processed data records received daily at the Archive to the expected number of data records. The results are tabulated by (1) individual datastream, site, and month for the current year and (2) site and fiscal year (FY) dating back to 1998. The U.S. Department of Energy (DOE) requires national user facilities to report time-based operating data. The requirements concern the actual hours of operation (ACTUAL); the estimated maximum operation or uptime goal (OPSMAX), which accounts for planned downtime; and the VARIANCE [1 - (ACTUAL/OPSMAX)], which accounts for unplanned downtime. The OPSMAX time for the first quarter of FY2010 for the Southern Great Plains (SGP) site is 2097.60 hours (0.95 x 2208 hours this quarter). The OPSMAX for the North Slope Alaska (NSA) locale is 1987.20 hours (0.90 x 2208) and for the Tropical Western Pacific (TWP) locale is 1876.80 hours (0.85 x 2208). The first ARM Mobile Facility (AMF1) deployment in Graciosa Island, the Azores, Portugal, continued through this quarter, so the OPSMAX time this quarter is 2097.60 hours (0.95 x 2208). The second ARM Mobile Facility (AMF2) began deployment this quarter to Steamboat Springs, Colorado. The experiment officially began November 15, but most of the instruments were up and running by November 1. Therefore, the OPSMAX time for the AMF2 was 1390.80 hours (.95 x 1464 hours) for November and December (61 days). The differences in OPSMAX performance reflect the complexity of local logistics and the frequency of extreme weather events. It is impractical to measure OPSMAX for each instrument or datastream. Data availability reported here refers to the average of the individual, continuous datastreams that have been received by the Archive. Data not at the Archive are caused by downtime (scheduled or unplanned) of the individual instruments. Therefore, data availability is directly related to individual instrument uptime. Thus, the average percentage of data in the Archive represents the average percentage of the time (24 hours per day, 92 days for this quarter) the instruments were operating this quarter. Summary. Table 1 shows the accumulated maximum operation time (planned uptime), actual hours of operation, and variance (unplanned downtime) for the period October 1-December 31, 2010, for the fixed sites. Because the AMFs operate episodically, the AMF statistics are reported separately and not included in the aggregate average with the fixed sites. This first quarter comprises a total of 2,208 possible hours for the fixed sites and the AMF1 and 1,464 possible hours for the AMF2. The average of the fixed sites exceeded our goal this quarter. The AMF1 has essentially completed its mission and is shutting down to pack up for its next deployment to India. Although all the raw data from the operational instruments are in the Archive for the AMF2, only the processed data are tabulated. Approximately half of the AMF2 instruments have data that was fully processed, resulting in the 46% of all possible data made available to users through the Archive for this first quarter. Typically, raw data is not made available to users unless specifically requested.

Sisterson, D. L.

2011-02-01T23:59:59.000Z

184

BOREAS TE-09 PAR & Leaf Nitrogen Data for NSA Revised</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">used the referenced data set before April 20, 2004, you should download it again from the ORNL DAAC. If you ordered the BOREAS CD-ROM set, you should contact our Users Services...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">185</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf12/extended_abs/widener2-kb.pdf"> <span id="translatedtitle">New ARM Data Stream: Surface Images at <span class="hlt">NSA</span>/AAO Sites in Barrow...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">delivered to the ARM archive. In Barrow, the camera resides at the top of the 40-meter tower. In Atqasuk, the camera is placed on a post attached to a piling near the 10-meter tip...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">186</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf13/extended_abs/shaw-ja.pdf"> <span id="translatedtitle">Short-Term Arctic Cloud Statistics at <span class="hlt">NSA</span> from the Infrared Cloud...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">J. A. Shaw and B. Thurairajah Department of Electrical and Computer Engineering Montana State University Bozeman, Montana Introduction The infrared cloud imager (ICI) is a...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">187</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/MWR3264.1"> <span id="translatedtitle">Evaluation of the NCEP Global Forecast System at the ARM <span class="hlt">SGP</span> Site</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">This study evaluates the performance of the National Centers for Environmental Prediction Global Forecast System (GFS) against observations made by the U.S. Department of Energy Atmospheric Radiation Measurement (ARM) Program at the southern ...</p> <div class="credits"> <p class="dwt_author">Fanglin Yang; Hua-Lu Pan; Steven K. Krueger; Shrinivas Moorthi; Stephen J. Lord</p> <p class="dwt_publisher"></p> <p class="publishDate">2006-12-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">188</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf12/extended_abs/cazull-seb.pdf"> <span id="translatedtitle">LandUse/Land Cover Map of the CF of ARM in the <span class="hlt">SGP</span> Site Using...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">the effects and interactions of sunlight, radiant energy, and clouds on temperatures, weather, and climate. (http:www.arm.govdocsabout.html) This energy balance is affected by...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">189</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/1525-7541%282003%29004%3C0106%3ASVISWF%3E2.0.CO%3B2"> <span id="translatedtitle">Spatiotemporal Variations in Soil Water: First Results from the ARM <span class="hlt">SGP</span> CART Network</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">A network of automated soil water and temperature systems, installed at 21 locations in Oklahoma and Kansas in 1996 and 1997, is providing hourly profiles of soil temperature and water at eight depths, from 0.05 to 1.75 m below the surface, in ...</p> <div class="credits"> <p class="dwt_author">J. M. Schneider; D. K. Fisher; R. L. Elliott; G. O. Brown; C. P. Bahrmann</p> <p class="dwt_publisher"></p> <p class="publishDate">2003-02-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">190</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/dataexplorer/details.jsp?id=1077237"> <span id="translatedtitle">Atmospheric Radiation Measurement (ARM) Data from the Southern Great Plains (<span class="hlt">SGP</span>) Site</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/dataexplorer/">DOE Data Explorer (OSTI) </a></p> <p class="result-summary">The Office of Biological and Environmental Research in DOE's Office of Science is responsible for the ARM Program. The ARM Archive physically resides at the Oak Ridge National Laboratory. (Specialized Interface) (Registration Required)</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">191</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/abs/10.1175/2011JCLI3978.1?prevSearch=%5BFulltext%3A+DOE+AND+Strategic+AND+Plan%5D&searchHistoryKey="> <span id="translatedtitle">A Comparison of MERRA and NARR Reanalyses with the DOE ARM <span class="hlt">SGP</span> Data</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">Atmospheric states from the Modern-Era Retrospective analysis for Research and Applications (MERRA) and the North American Regional Reanalysis (NARR) are compared with data from the Atmospheric Radiation Measurement Program (ARM) Southern Great ...</p> <div class="credits"> <p class="dwt_author">Aaron D. Kennedy; Xiquan Dong; Baike Xi; Shaocheng Xie; Yunyan Zhang; Junye Chen</p> <p class="dwt_publisher"></p> <p class="publishDate">2011-09-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">192</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/2007JCLI2266.1"> <span id="translatedtitle">Temporal Variability of Fair-Weather Cumulus Statistics at the ACRF <span class="hlt">SGP</span> Site</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">Continental fair-weather cumuli exhibit significant diurnal, day-to-day, and year-to-year variability. This study describes the climatology of cloud macroscale properties, over the U.S. Department of Energys Atmospheric Radiation Measurement (...</p> <div class="credits"> <p class="dwt_author">Larry K. Berg; Evgueni I. Kassianov</p> <p class="dwt_publisher"></p> <p class="publishDate">2008-07-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">193</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/abs/10.1175/1520-0493%282003%29131%3C0926%3AEMMPOC%3E2.0.CO%3B2?prevSearch=%5BFulltext%3A+DOE+AND+virtual+AND+university%5D&searchHistoryKey="> <span id="translatedtitle">Evaluating Mesoscale Model Predictions of Clouds and Radiation with <span class="hlt">SGP</span> ARM Data over a Seasonal Timescale</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">This study evaluates the predictions of radiative and cloud-related processes of the fifth-generation Pennsylvania State UniversityNational Center for Atmospheric Research (PSUNCAR) Mesoscale Model (MM5). It is based on extensive comparison of ...</p> <div class="credits"> <p class="dwt_author">Franoise Guichard; David B. Parsons; Jimy Dudhia; James Bresch</p> <p class="dwt_publisher"></p> <p class="publishDate">2003-05-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">194</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00142.pdf"> <span id="translatedtitle">Preliminary Analysis of ARM <span class="hlt">SGP</span> Area Sky Cover and Downwelling SW Irradiance</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Clarifying and Implementing a Stricter DOD Definition Across Datastreams Clarifying and Implementing a Stricter DOD Definition Across Datastreams C. Sivaraman, B. Ermold, M. Macduff Pacific Northwest National Laboratory Definition of DOD: All dimension, attribute and variable types and names are considered part of a DOD. A change in any part of the DOD is considered a version change. Outcomes: ACRF enforces greater consistency in data Downstream users benefit (DQ, VAPs, scientists) Identify inconsistencies across datastreams Datastream development is more efficient BODS interface, updated libraries Improved data analysis tools for ACRF and ARM Visual Datastream history tool (below) Issues with current DOD history: The DOD History page: http://science.arm.gov/tool/dod/showdod.php * Tracks both content and structure. * Needs Custom Configuration </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">195</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/poster_abs/P00150"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Infrared Interferometric Measurements of the Air-Sea Temperature Difference Infrared Interferometric Measurements of the Air-Sea Temperature Difference Minnett, P.J., Rosenstiel School of Marine and Atmospheric Science, University of Miami Eleventh Atmospheric Radiation Measurement (ARM) Science Team Meeting Marine Atmosphere Emitted Radiance Interferometers (M-AERI) have been mounted on several research ships on cruises in the world?s oceans, several in the areas of the ARM <span class="hlt">TWP</span> and <span class="hlt">NSA</span>-AAO sites. Accurate measurements of the skin sea-surface temperature and near-surface air temperatures are derived from the infrared spectral measurements, which, unlike conventional measurements of air-sea temperature difference, have a common calibration. This removes the largest source of uncertainty in the measurement of air-sea temperature differences, and thereby a major uncertainty in </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">196</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf15/extended_abs/ritsche_mt.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">and Improved Data Logging and Collection and Improved Data Logging and Collection System for Atmospheric Radiation Measurement Climate Research Facility, Tropical Western Pacific, and North Slope of Alaska Sky Radiation, Ground Radiation, and MET Systems M.T. Ritsche, D.J. Holdridge Environmental Research Division, Argonne National Laboratory Argonne, IL R. Pearson Australian Bureau of Meteorology Darwin, NT Australia Background Aging systems and technological advances mandated changes to the data collection systems at the Atmospheric Radiation Measurement (ARM) Program's Tropical Western Pacific (<span class="hlt">TWP</span>) and North Slope of Alaska (<span class="hlt">NSA</span>) ARM Climate Research Facility (ACRF) sites. Key reasons for the upgrade include the following: * Achieve consistency across all ACRF sites for easy data use and operational maintenance. </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">197</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/dataexplorer/details.jsp?id=1081515"> <span id="translatedtitle">ARM Multi-Filter Rotating Shadowband Radiometer (MFRSR): irradiances</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/dataexplorer/">DOE Data Explorer (OSTI) </a></p> <p class="result-summary">The multifilter rotating shadowband radiometer (MFRSR) takes spectral measurements of direct normal, diffuse horizontal and total horizontal solar irradiances. These measurements are at nominal wavelengths of 415, 500, 615, 673, 870, and 940 nm. The measurements are made at a user-specified time interval, usually about one minute or less. The sampling rate for the Atmospheric Radiation Measurement (ARM) Climate Research Facility MFRSRs is 20 seconds. From such measurements, one may infer the atmosphere's optical depth at the wavelengths mentioned above. In turn, these optical depths may be used to derive information about the column abundances of ozone and water vapor (Michalsky et al. 1995), as well as aerosol (Michalsky et al. 1994) and other atmospheric constituents. A silicon detector is also part of the MFRSR. This detector provides a measure of the broadband direct normal, diffuse horizontal and total horizontal solar irradiances. A MFRSR head that is mounted to look vertically downward can measure upwelling spectral irradiances. In the ARM system, this instrument is called a multifilter radiometer (MFR). At the Southern Great Plains (<span class="hlt">SGP</span>) there are two MFRs; one mounted at the 10-m height and the other at 25 m. At the North Slope of Alaska (<span class="hlt">NSA</span>) sites, the MFRs are mounted at 10 m. MFRSR heads are also used to measure normal incidence radiation by mounting on a solar tracking device. These are referred to as normal incidence multi-filter radiometers (NIMFRs) and are located at the <span class="hlt">SGP</span> and <span class="hlt">NSA</span> sites. Another specialized use for the MFRSR is the narrow field of view (NFOV) instrument located at <span class="hlt">SGP</span>. The NFOV is a ground-based radiometer (MFRSR head) that looks straight up.</p> <div class="credits"> <p class="dwt_author">Hodges, Gary</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">198</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/data/eval/69"> <span id="translatedtitle">ARM - Evaluation Product - Corrected Moments in Antenna Coordinates</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">ProductsCorrected Moments in Antenna Coordinates ProductsCorrected Moments in Antenna Coordinates Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Evaluation Product : Corrected Moments in Antenna Coordinates Site(s) <span class="hlt">SGP</span> <span class="hlt">TWP</span> General Description Raw moments from the scanning ARM precipitation radars (SAPRs) are subject to a number of instrumental and atmospheric phenomena that must be retrieved and corrected for. The Corrected Moments in Antenna Coordinates (CMAC) value-added product contains both raw data and fields that have been processed to: · correct for velocity aliasing · unfold and generate a cross-polarimetric phase difference that is monotonically increasing, removing impulses caused by non-uniform beam filling and phase shift on backscatter · recalculate specific differential phase using a 20-point Sobel filter on </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">199</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/meetings/2009/presentations/0330/6_Kassianov_AWG2009.pdf"> <span id="translatedtitle">Slide 1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Kassianov Kassianov Aerosol remote sensing under partly cloudy conditions: How well are we doing? Background Ground-based/airborne lidar observations: Raman Lidar (RL), Micropulse Lidar (MPL) High Spectral Resolution Lidar (HSRL) Can they be extended by other observations? Outline Q1: Why it is important? Q2: What issues do we have? Q3: How can we address them? Q1: IAE and Aerosol RF Simultaneous and coincident measurements of aerosol and cloud properties are desirable: Indirect Aerosol Effects (IAEs) Aerosol Radiative Forcing (RF) Ghan and Schwartz, BAMS, 2007 Myhre et al., ACP, 2009 Q1: Occurrence Partly cloudy sky: 30% (<span class="hlt">SGP</span>), 40-80% (<span class="hlt">TWP</span>) Credit: C. Long Q2: 3D Problem Examples of 3D Cloud Impacts: Positive Cloud Radiative Forcing (RF) Reflectance Enhancement Cloud Screening Q2: Positive Cloud RF </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">200</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/data/eval/57"> <span id="translatedtitle">ARM - Evaluation Product - Interpolated Sonde</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">ProductsInterpolated Sonde ProductsInterpolated Sonde Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Evaluation Product : Interpolated Sonde Site(s) GAN <span class="hlt">SGP</span> <span class="hlt">TWP</span> General Description The interpolated-sonde value-added product is a modification of the mergesonde VAP that produces a daily file of thermodynamic variables from radiosonde soundings, the microwave radiometer, and surface meteorological instruments. This product does not incorporate ECMWF model output. Interpolated-sonde includes many of the same sophisticated scaling/interpolation/smoothing schemes that are the hallmark of the mergesonde VAP, but there are benefits to excluding ECMWF model output. These benefits include (1) a shorter time lag in producing a thermodynamic profile, and (2) the profiles are independent of the model so comparisons </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_9");' href="#" title="Previous Page"> <img id="PreviousPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.previous.18x20.png" alt="Previous Page" /></a> <span id="PageLinks" class="pageLinks"> <span> <a onClick='return 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twp</strong> from the National Library of Energy <sup>Beta</sup> (NLE<sup>Beta</sup>)</h2> </div> <center><strong>Note: This page contains sample records for the topic "nsa sgp twp" from the National Library of Energy<sup>Beta</sup> (NLE<sup>Beta</sup>).<br> While these samples are representative of the content of NLE<sup>Beta</sup>,<br> they are not comprehensive nor are they the most current set.<br> We encourage you to perform a <a href="http://www.osti.gov/nle">real-time search of NLE<sup>Beta</sup></a><br> to obtain the most current and comprehensive results.</strong></center><p><br></p> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" 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class="Icon" src="http://www.osti.gov/nlesearch/images/icon.last.18x20.png" alt="Last Page" /></a> </div> <a href="http://www.osti.gov/nle/topicpages">Index</a> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">201</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf12/extended_abs/gaustad-kl.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Evaluation of Cloud Cover, Cloud Effect, and Surface Evaluation of Cloud Cover, Cloud Effect, and Surface Radiation Budgets at the <span class="hlt">SGP</span> and <span class="hlt">TWP</span> ARM Sites K. L. Gaustad and C. N. Long Pacific Northwest National Laboratory Richland, Washington Introduction The U.S. Department of Energy (DOE) Atmospheric Radiation Measurement (ARM) Program has established networks of broadband shortwave (SW) radiometers at each of its field research sites. The shortwave flux analysis value-added product (SWFuxAnal VAP) applies a clear-sky detection and fitting technique to data collected from these sensors to identify clear-sky conditions, produce a continuous estimate of clear-sky SW irradiance, and assess the effect of cloudiness on downwelling SW measurements. The clear-sky detection algorithm has been expanded to allow its use in not only </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">202</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf08/extended_abs/ayers_jk.pdf"> <span id="translatedtitle">ayers-98.pdf</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Calibration of Geostationary Satellite Imager Calibration of Geostationary Satellite Imager Data for ARM Using AVHRR J. K. Ayers, L. Nguyen, and W. L. Smith, Jr. Analytical Services and Materials, inc. Hampton, Virginia P. Minnis Atmospheric Sciences Division NASA-Langley Research Center Hampton, Virginia Introduction Geostationary satellite imager data are a key part of the Atmospheric Radiation Measurement (ARM) Program. They complement the suite of surface measurements taken at the Southern Great Plains (<span class="hlt">SGP</span>) and the Tropical Western Pacific (<span class="hlt">TWP</span>) sites. The data are used to derive cloud prop- erties and the top-of-the-atmosphere radiation budget at sev- eral time and space scales. Retrievals of cloud and radiative properties from satellite imager data require accurate cali- bration of the various channels and satellites used in the </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">203</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf14/extended_abs/rutan-da.pdf"> <span id="translatedtitle">Validation of CERES/SARB Data Product Using ARM Surface Flux Observations</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">CERES/SARB Data Product Using CERES/SARB Data Product Using ARM Surface Flux Observations D. A. Rutan Analytical Services and Materials Inc. Hampton, Virginia T. P. Charlock National Aeronautics and Space Administration Langley Research Center Hampton, Virginia Introduction This paper uses surface observed broadband fluxes from Atmospheric Radiation Measurement (ARM) Southern Great Plains (<span class="hlt">SGP</span>), ARM Tropical Western Pacific (<span class="hlt">TWP</span>), and a number of other sites to validate model results from the Clouds and the Earth's Radiant Energy System (CERES) Surface and Radiation Budget (SARB) Clouds and Radiative Swath (CRS) data products during the months of January-December 2001. CERES instruments fly aboard the Terra and Aqua satellites measuring broadband radiation in three channels: total (0.3-∝ µm), shortwave (0.3-5.0 µm), and window </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">204</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/data/eval/70"> <span id="translatedtitle">ARM - Evaluation Product - Quantitative Precipitation Estimates (QPE) from</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">ProductsQuantitative Precipitation Estimates (QPE) ProductsQuantitative Precipitation Estimates (QPE) from the CSAPR Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Evaluation Product : Quantitative Precipitation Estimates (QPE) from the CSAPR Site(s) <span class="hlt">SGP</span> <span class="hlt">TWP</span> General Description Precipitation rates from cloud systems can give a fundamental insight into the processes occurring in-cloud. While rain gauges and disdrometers can give information at a single point, remote sensors such as radars can provide rainfall information over a defined area. The QPE value-added product (VAP) takes the Corrected Moments in Antenna Coordinates VAP and maps the Rain_rate_A field onto a Cartesian grid at the surface. This field is the rain rate as determined using the specific attenuation (A, dBZ/km) due to two-way liquid attenuation after Ryzhkov et </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">205</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/data/pi/17"> <span id="translatedtitle">ARM - PI Product - Large Scale Ice Water Path and 3-D Ice Water Content</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">ProductsLarge Scale Ice Water Path and 3-D Ice Water ProductsLarge Scale Ice Water Path and 3-D Ice Water Content Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send PI Product : Large Scale Ice Water Path and 3-D Ice Water Content Site(s) <span class="hlt">SGP</span> <span class="hlt">TWP</span> General Description Cloud ice water concentration is one of the most important, yet poorly observed, cloud properties. Developing physical parameterizations used in general circulation models through single-column modeling is one of the key foci of the ARM program. In addition to the vertical profiles of temperature, water vapor and condensed water at the model grids, large-scale horizontal advective tendencies of these variables are also required as forcing terms in the single-column models. Observed horizontal advection of condensed water has not been available because the </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">206</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf08/extended_abs/shields_je.pdf"> <span id="translatedtitle">shields-98.pdf</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">7 7 The Whole Sky Imager - A Year of Progress J. E. Shields and M. E. Karr Marine Physical Laboratory Scripps Institution of Oceanography University of California, San Diego San Diego, California T. P. Tooman Sandia National Laboratories Livermore, California D. H. Sowle and S. T. Moore Mission Research Corporation Santa Barbara, California Abstract Much progress has been made this last year in realizing the potential of the whole sky imager (WSI). Two imagers are deployed [at the Southern Great Plains (<span class="hlt">SGP</span>) site and the Surface Heat Budget of the Arctic Ocean (SHEBA)], two are being prepared for deployment in the Tropical Western Pacific (<span class="hlt">TWP</span>), and more are in production. Data products now include daytime thick cloud fraction and calibrated radiance. Night cloud fraction and daytime thin cloud </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">207</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/data/eval/55"> <span id="translatedtitle">ARM - Evaluation Product - Mapped Moments to a Cartesian Grid</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">ProductsMapped Moments to a Cartesian Grid ProductsMapped Moments to a Cartesian Grid Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Evaluation Product : Mapped Moments to a Cartesian Grid Site(s) <span class="hlt">SGP</span> <span class="hlt">TWP</span> General Description The Scanning ARM precipitation radars produce measurements of raw radar moments in antenna coordinates of range from and the azimuth and elevation of the antenna. Most numerical representations of the atmosphere tend to be in a Cartesian coordinate system using either height above mean sea level (or land surface in sigma coordinates) or pressure levels as a vertical scale. In addition to applying a correction for radar aliasing, correcting cross polarimetric phase difference for second trip returns and folding, recalculating specific differential phase (due to a configuration error on </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">208</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/highlights/RMjY5/view"> <span id="translatedtitle">Research Highlight</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Estimating the Ice Crystal Enhancement Factor in the Tropics Estimating the Ice Crystal Enhancement Factor in the Tropics Download a printable PDF Submitter: Zeng, X., NASA - Goddard Space Flight Center Tao, W., NASA - Goddard Space Flight Center Area of Research: General Circulation and Single Column Models/Parameterizations Working Group(s): Cloud Life Cycle, Cloud-Aerosol-Precipitation Interactions Journal Reference: Zeng X, W Tao, T Matsui, S Xie, S Lang, M Zhang, DO Starr, and X Li. 2011. "Estimating the ice crystal enhancement factor in the tropics." Journal of the Atmospheric Sciences, 68(7), doi:10.1175/2011JAS3550.1. Figure 1. Twenty-day mean vertical profiles of IWC from the ARM-<span class="hlt">SGP</span> observations and the three simulations using low, moderate, and high ice crystal concentrations, respectively. Figure 2. Eight-day mean vertical profiles of IWC from the <span class="hlt">TWP</span>-ICE </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">209</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/1054629"> <span id="translatedtitle">C-Band Scanning ARM Precipitation Radar (C-SAPR) Handbook</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">The C-band scanning ARM precipitation radar (C-SAPR) is a scanning polarimetric Doppler radar transmitting simultaneously in both H and V polarizations. With a 350-kW magnetron transmitter, this puts 125 kW of transmitted power for each polarization. The receiver for the C-SAPR is a National Center for Atmospheric Research (NCAR) -developed Hi-Q system operating in a coherent-on-receive mode. The ARM Climate Research Facility operates two C-SAPRs; one of them is deployed near the Southern Great Plains (<span class="hlt">SGP</span>) Central Facility near the triangular array of X-SAPRs, and the second C-SAPR is deployed at ARMs Tropical Western Pacific (<span class="hlt">TWP</span>) site on Manus Island in Papua New Guinea.</p> <div class="credits"> <p class="dwt_author">Widener, K; Bharadwaj, N</p> <p class="dwt_publisher"></p> <p class="publishDate">2012-11-13T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">210</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://escholarship.org/uc/item/0sp582mq?query=space+AND+propulsion"> <span id="translatedtitle">Comparison of improved Aura Tropospheric Emission Spectrometer (TES) CO2 with HIPPO and <span class="hlt">SGP</span> aircraft profile measurements</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">Propulsion Laboratory, California Institute of Technology, was performed under a contract with the National Aeronautics and Space</p> <div class="credits"> <p class="dwt_author">Kulawik, S.S.</p> <p class="dwt_publisher"></p> <p class="publishDate">2013-01-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">211</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://escholarship.org/uc/item/0sp582mq?query=carbon+AND+dioxide"> <span id="translatedtitle">Comparison of improved Aura Tropospheric Emission Spectrometer (TES) CO2 with HIPPO and <span class="hlt">SGP</span> aircraft profile measurements</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">Aircraft observation of carbon dioxide at 8-13km altitudedecade, measurements of carbon dioxide (CO ) from space haveEmission Spectrome- ter (TES) carbon dioxide (CO ) satellite</p> <div class="credits"> <p class="dwt_author">Kulawik, S.S.</p> <p class="dwt_publisher"></p> <p class="publishDate">2013-01-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">212</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/abs/10.1175/1520-0450%282000%29039%3C0971%3ASRODTS%3E2.0.CO%3B2?prevSearch=%5BFulltext%3A+Windows%5D&searchHistoryKey="> <span id="translatedtitle">Simultaneous Retrieval of Diurnal to Seasonal Surface Temperatures and Emissivities over <span class="hlt">SGP</span> ARMCART Site Using GOES Split Window</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">GOES-8 thermal infrared split window measurements have been used with a simultaneous land surface temperature (LST)spectral emissivity retrieval algorithm to examine the potential of a combined retrieval methodology cast into a variational ...</p> <div class="credits"> <p class="dwt_author">David A. Faysash; Eric A. Smith</p> <p class="dwt_publisher"></p> <p class="publishDate">2000-07-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">213</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/data/eval/1"> <span id="translatedtitle">ARM - Evaluation Product - Multispectral Thermal Imager (MTI)</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">ProductsMultispectral Thermal Imager (MTI) ProductsMultispectral Thermal Imager (MTI) Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Evaluation Product : Multispectral Thermal Imager (MTI) 2000.10.01 - 2003.05.02 Site(s) <span class="hlt">NSA</span> <span class="hlt">SGP</span> General Description The Multispectral Thermal Imager is a space-based research and development project sponsored by the U.S. Department of Energy (DOE), Office of Nonproliferation and National Security. MTI's primary objective is to demonstrate advanced multispectral and thermal imaging, image processing, and associated technologies that could be used in future systems for detecting and characterizing facilities producing weapons of mass destruction. However, ARM and the MTI have an arrangement that allows ARM to receive MTI images. </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">214</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf14/poster_abs/P00041"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Understanding the Effects of Uncertainties in Ice Processes, Entrainment Understanding the Effects of Uncertainties in Ice Processes, Entrainment and Updraft Velocities on the Relationship Between Cloud Optical Depth and Liquid Water Path at the <span class="hlt">NSA</span> and <span class="hlt">SGP</span> Sites Chen, Y.(a), Penner, J.E.(a), and Dong, X.(b), University of Michigan (a), University of North Dakota (b) The relationship between the cloud optical depth (tc) and the cloud liquid water path (LWP) inferred from surface observations of shortwave radiative fluxes and measured LWP shows significant variability. Our previous study1 used a warm-cloud microphysics model to explain the average relationship between the cloud optical depth (tc) and the cloud liquid water path (LWP). Here, we examine some of the processes that contribute to the observed variability in this relationship. We examine the possible effects of </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">215</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf15/extended_abs/somerville_rcj.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Single-Column Modeling, GCM Parameterizations and Single-Column Modeling, GCM Parameterizations and Atmospheric Radiation Measurement Data R.C.J. Somerville and S.F. Iacobellis Scripps Institution of Oceanography/USCD La Jolla, California Introduction Our overall goal is identical to that of the Atmospheric Radiation Measurement (ARM) Program: the development of new and improved parameterizations of cloud-radiation effects and related processes, using ARM data at all three ARM sites, and the implementation and testing of these parameterizations in global and regional models. To test recently developed prognostic parameterizations based on detailed cloud microphysics, we have first compared single-column model (SCM) output with ARM observations at the Southern Great Plains (<span class="hlt">SGP</span>), North Slope of Alaska (<span class="hlt">NSA</span>) and Topical Western </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">216</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/poster_abs/P00190"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">International Pyrgeometer and Absolute Sky-scanning Radiometer Comparison International Pyrgeometer and Absolute Sky-scanning Radiometer Comparison at the <span class="hlt">NSA</span> ARM site Barrow Stamnes, K. (a), Dutton, E.G. (b), Marty, Ch. (c), Michalsky, J.J. (d), Philipona, R. (e), Stoffel, T. (f), Storvold, R. (c), and Zak, B.D. (g), Stevens Institute of Technology, New Jersey (a), NOAA, Climate Monitoring and Diagnostics Laboratory (b), University of Alaska Fairbanks (c), State University of New York at Albany (d), World Radiation Center, Davos, Switzerland (e), National Renewable Energy Lab, Boulder (f), Sandia National Laboratories, Albuquerque (g) Eleventh Atmospheric Radiation Measurement (ARM) Science Team Meeting The first International Prgeometer and Absolute Sky-scanning Radiometer Comparison (IPASRC I), which was held in fall 1999 at the ARM <span class="hlt">SGP</span> site in </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">217</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/highlights/RMjM3/view"> <span id="translatedtitle">Research Highlight</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Field Experiments to Improve the Treatment of Radiation in the Mid-to-Upper Field Experiments to Improve the Treatment of Radiation in the Mid-to-Upper Troposphere Download a printable PDF Submitter: Turner, D. D., National Oceanic and Atmospheric Administration Mlawer, E. J., Atmospheric & Environmental Research, Inc. Area of Research: Radiation Processes Working Group(s): Cloud-Aerosol-Precipitation Interactions Journal Reference: Turner DD and EJ Mlawer. 2010. "The Radiative Heating in Underexplored Bands Campaigns (RHUBC)." Bulletin of the American Meteorological Society, 91, doi:10.1175/2010BAMS2904.1. (a) Atmospheric transmittance at 1 cm-1 resolution in the far-infrared for three atmospheres that are representative of the ARM <span class="hlt">SGP</span> site, <span class="hlt">NSA</span> site, and RHUBC-II site in the Chajnantor plateau (CJC). (b) The transmittance </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">218</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf16/extended_abs/zhuravleva_tb.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Cloud Amount of Midlatitude Continental Cloud Amount of Midlatitude Continental Clouds in Tomsk Region: Preliminary Results T.B. Zhuravleva, T.M. Rasskazchikova, and T.K. Sklyadneva Institute of Atmospheric Optics SB RAS Tomsk, Russia S.V. Smirnov Institute of Monitoring of Climatic and Ecological Systems SB RAS Tomsk, Russia The Atmospheric Radiation Measurement (ARM) Program provides concentrated measurements of surface radiative budget as well as measurements of the atmospheric constituents including clouds, aerosols, water vapor, etc. at the Southern Great Plains (<span class="hlt">SGP</span>), the Tropical Western Pacific and the North Slope of Alaska (<span class="hlt">NSA</span>) sites. The data obtained allow studying a wide, but not the full range of climatologically relevant possibilities, and thus additional investigations are needed to provide the </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">219</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/1523"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">New Data Stream Available from Millimeter Wave Cloud Radar New Data Stream Available from Millimeter Wave Cloud Radar Bookmark and Share Inside the instrument shelter, the MMCR data system collects radar spectral data and processes these into reflectivity, vertical velocities, and spectral width. Inside the instrument shelter, the MMCR data system collects radar spectral data and processes these into reflectivity, vertical velocities, and spectral width. As a result of upgrades to the Millimeter Wave Cloud Radar (MMCR) processors (see http://www.arm.gov/acrf/updates051504.stm#nsammcr) at the ARM Climate Research Facility Southern Great Plains (<span class="hlt">SGP</span>) and North Slope of Alaska (<span class="hlt">NSA</span>) locales, two MMCR data streams-mmcrcalC1.a1 (calibration data) and mmcrmomentsC1.a1 (spectral "moments" data)-have been combined </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">220</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/meetings/2009/presentations/0330/6_JeffersonSTM09.pdf"> <span id="translatedtitle">JeffersonSTM09.ppt</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">AOS: Measurements of Aerosol Optical and AOS: Measurements of Aerosol Optical and AOS: Measurements of Aerosol Optical and Cloud-forming Properties Cloud-forming Properties Anne Jefferson and John Ogren NOAA Environmental Science Research Laboratory CIRES, University of Colorado ARM STM 2009 Aerosol Observing Systems In-situ surface measurements of aerosol optical, chemical, size, hygroscopic and cloud-forming properties * <span class="hlt">SGP</span> - ARM central facility Lamont, OK *AMF - Pt Reyes, CA 3/2005 - 9/2005 - Niamey, Niger 12/2005-1/2007 - Murg Valley, Germany 4/2007 -1/2008 - Shouxian China 5/2008 - 12/2008 - Graciosa Island, Azores 4/2009 *BRW/<span class="hlt">NSA</span> - Barrow Alaska *AMF2 ? Darwin? - What instruments support the science? AMF deployment in Shouxian China, HFE HFE was located at a rural, agricultural area ~120 km from Hefei, ~200 km from Nanking </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_10");' href="#" title="Previous Page"> <img id="PreviousPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.previous.18x20.png" alt="Previous Page" /></a> <span id="PageLinks" class="pageLinks"> <span> <a onClick='return showDiv("page_1");' 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class="Icon" src="http://www.osti.gov/nlesearch/images/icon.last.18x20.png" alt="Last Page" /></a> </div> <a href="http://www.osti.gov/nle/topicpages">Index</a> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">221</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/2010JAMC2401.1"> <span id="translatedtitle">Obtaining Best Estimates for the Microphysical and Radiative Properties of Tropical Ice Clouds from <span class="hlt">TWP</span>-ICE In Situ Microphysical Observations</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">Best estimates of the bulk microphysical and radiative properties (ice water content, visible extinction, effective radius, and total concentration) are derived for three case studies of tropical ice clouds sampled during the Tropical Warm Pool ...</p> <div class="credits"> <p class="dwt_author">A. Protat; G. M. McFarquhar; J. Um; J. Delano</p> <p class="dwt_publisher"></p> <p class="publishDate">2011-04-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">222</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/servlets/purl/972321"> <span id="translatedtitle">Evaluating cloud retrieval algorithms with the ARM BBHRP framework</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">Climate and weather prediction models require accurate calculations of vertical profiles of radiative heating. Although heating rate calculations cannot be directly validated due to the lack of corresponding observations, surface and top-of-atmosphere measurements can indirectly establish the quality of computed heating rates through validation of the calculated irradiances at the atmospheric boundaries. The ARM Broadband Heating Rate Profile (BBHRP) project, a collaboration of all the working groups in the program, was designed with these heating rate validations as a key objective. Given the large dependence of radiative heating rates on cloud properties, a critical component of BBHRP radiative closure analyses has been the evaluation of cloud microphysical retrieval algorithms. This evaluation is an important step in establishing the necessary confidence in the continuous profiles of computed radiative heating rates produced by BBHRP at the ARM Climate Research Facility (ACRF) sites that are needed for modeling studies. This poster details the continued effort to evaluate cloud property retrieval algorithms within the BBHRP framework, a key focus of the project this year. A requirement for the computation of accurate heating rate profiles is a robust cloud microphysical product that captures the occurrence, height, and phase of clouds above each ACRF site. Various approaches to retrieve the microphysical properties of liquid, ice, and mixed-phase clouds have been processed in BBHRP for the ACRF Southern Great Plains (<span class="hlt">SGP</span>) and the North Slope of Alaska (<span class="hlt">NSA</span>) sites. These retrieval methods span a range of assumptions concerning the parameterization of cloud location, particle density, size, shape, and involve different measurement sources. We will present the radiative closure results from several different retrieval approaches for the <span class="hlt">SGP</span> site, including those from Microbase, the current 'reference' retrieval approach in BBHRP. At the <span class="hlt">NSA</span>, mixed-phase clouds and cloud with a low optical depth are prevalent; the radiative closure studies using Microbase demonstrated significant residuals. As an alternative to Microbase at <span class="hlt">NSA</span>, the Shupe-Turner cloud property retrieval algorithm, aimed at improving the partitioning of cloud phase and incorporating more constrained, conditional microphysics retrievals, also has been evaluated using the BBHRP data set.</p> <div class="credits"> <p class="dwt_author">Mlawer,E.; Dunn,M.; Mlawer, E.; Shippert, T.; Troyan, D.; Johnson, K. L.; Miller, M. A.; Delamere, J.; Turner, D. D.; Jensen, M. P.; Flynn, C.; Shupe, M.; Comstock, J.; Long, C. N.; Clough, S. T.; Sivaraman, C.; Khaiyer, M.; Xie, S.; Rutan, D.; Minnis, P.</p> <p class="dwt_publisher"></p> <p class="publishDate">2008-03-10T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">223</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://daac.ornl.gov/BOREAS/boreas_photos_pages/NSA-Airport_Photos.htm"> <span id="translatedtitle">BOREAS Operations</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Study Area Operations/Thompson Airport (<span class="hlt">NSA</span>-Ops) Study Area Operations/Thompson Airport (<span class="hlt">NSA</span>-Ops) <span class="hlt">NSA</span> Operations (<span class="hlt">NSA</span>-Ops) The Keewatin Air Hanger: site of BOREAS Ops 1994 Dr. Piers Sellers working in Ops, 1994 BOREAS "Air Force" The NASA C-130 The University of Wyoming King Air The NASA Helicopter The NRC Twin Otter The NCAR Electra The Ontario Chieftain Back to the BOREAS Photo Page Index Other Sites: <span class="hlt">NSA</span> Photos ||<span class="hlt">NSA</span>-BP Photos | <span class="hlt">NSA</span>-Fen Photos | <span class="hlt">NSA</span>-OA Photos | <span class="hlt">NSA</span>-OBS Photos | <span class="hlt">NSA</span>-OJP Photos | <span class="hlt">NSA</span>-UBS Photos | <span class="hlt">NSA</span>-YJP Photos | <span class="hlt">NSA</span>-Ops Photos SSA Photos || SSA-Airport Photos | SSA-Fen Photos | SSA-Mix Photos | SSA-OA Photos | SSA-OBS Photos | SSA-OJP Photos | SSA-YA Photos | SSA-YJP Photos | SSA-Ops Photos | ORNL DAAC Home || ORNL Home || NASA || Privacy, Security, Notices || Data Citation || Rate Us || Help | </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">224</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00122.pdf"> <span id="translatedtitle">Comparison of Cloud Fraction and Liquid Water Path between ECMWF simulations and ARM long-term Observations at the <span class="hlt">NSA</span> Site </span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">this poster, seasonal and annual variations of this poster, seasonal and annual variations of cloudiness and liquid water path (LWP) from European Center for Medium-Range Weather Forecasts (ECMWF) model were compared with surface measurement from the ARM Climate Research Facility (ARCF) North Slope of Alaska ( N S A ) s i t e b e t we e n J a n u a r y 1 9 9 9 and December 2004. ● Model simulated large scale features match well with observations. ● There are significant differences in cloud vertical and temporal distributions and in the magnitude. FIG. 1: Time-height display of cloud fraction from model simulations and observations in September 1999. ● Model overestimates high clouds, especially in warm seasons. ● Model makes close estimation for middle clouds. ● Model underestimates low clouds in warm seasons, especially in </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">225</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/data/time"> <span id="translatedtitle">ARM - Time in ARM NetCDF Files</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">govDataTime in ARM NetCDF Files govDataTime in ARM NetCDF Files Page Contents Introduction Time Zones Epoch Time Time Variables Conversion Examples and Hints Perl Example C Example Fortran Example IDL Example Notes on Generating Epoch Times Contact Information Time in ARM NetCDF Files Introduction This document explains most of the issues related to the use of time in ARM netCDF data files. Time Zones All ARM netCDF files are in UTC. Note that this has some implications for solar-based data; we tend to split our files at midnight, but the sun is still up at 0000 UTC at <span class="hlt">SGP</span> in the late spring and summer, and all the time at <span class="hlt">TWP</span>. This means a given solar arc may be broken across two different files. That's just the way it is; using local time in ARM files would have been a bigger mess. Note that splitting files at 0000 UTC is not an ARM standard, and many </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">226</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/JCLI3342.1"> <span id="translatedtitle">A Climatology of Midlatitude Continental Clouds from the ARM <span class="hlt">SGP</span> Central Facility: Part I: Low-Level Cloud Macrophysical, Microphysical, and Radiative Properties</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">A record of single-layer and overcast low cloud (stratus) properties has been generated using approximately 4000 h of data collected from January 1997 to December 2002 at the Atmospheric Radiation Measurement (ARM) Southern Great Plains Central ...</p> <div class="credits"> <p class="dwt_author">Xiquan Dong; Patrick Minnis; Baike Xi</p> <p class="dwt_publisher"></p> <p class="publishDate">2005-05-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">227</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/2007JCLI1987.1"> <span id="translatedtitle">The Vertical Structure of Cloud Occurrence and Radiative Forcing at the <span class="hlt">SGP</span> ARM Site as Revealed by 8 Years of Continuous Data</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">Data collected at the Atmospheric Radiation Measurement (ARM) Program ground sites allow for the description of the atmospheric thermodynamic state, cloud occurrence, and cloud properties. This information allows for the derivation of estimates ...</p> <div class="credits"> <p class="dwt_author">Gerald G. Mace; Sally Benson</p> <p class="dwt_publisher"></p> <p class="publishDate">2008-06-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">228</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/1520-0469%281997%29054%3C1289%3ASSRFAC%3E2.0.CO%3B2"> <span id="translatedtitle">Surface Solar Radiation Flux and Cloud Radiative Forcing for the Atmospheric Radiation Measurement (ARM) Southern Great Plains (<span class="hlt">SGP</span>): A Satellite, Surface Observations, and Radiative Transfer Model Study</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">This study presents surface solar radiation flux and cloud radiative forcing results obtained by using a combination of satellite and surface observations interpreted by means of a simple plane-parallel radiative transfer model called 2001. This ...</p> <div class="credits"> <p class="dwt_author">Catherine Gautier; Martin Landsfeld</p> <p class="dwt_publisher"></p> <p class="publishDate">1997-05-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">229</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00088.pdf"> <span id="translatedtitle">Microsoft PowerPoint - arm_stm_poster_2007_carl [Compatibility...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">SG Aerosol and Water Vapor Measurements Acquired by the Upgraded <span class="hlt">SGP</span> Raman Lidar During ALIVE Aerosol and Water Vapor Measurements Acquired by the Upgraded <span class="hlt">SGP</span> Raman Lidar During...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">230</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.ecd.bnl.gov/pubs/BNL-80211-2008-AB.pdf"> <span id="translatedtitle">HISTORY AND CURRENT STATUS OF THE CIMEL SUN-PHOTOMETERS AT ACRF SITES</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">, Tropical Western Pacific [<span class="hlt">TWP</span>]-C2, the ARM Mobile Facility [AMF]). This comes on the heels of two important</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">231</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/sites/prod/files/CX-004500.pdf"> <span id="translatedtitle">NETL F 451.1-1/1 Categorical Exclusion (CX) Designation Form</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">PMCBETD 2010 Gary Sames 8162010 - 2162012 Cranberry <span class="hlt">Twp</span>, PA Energy and Daylighting Demonstration & Assessment of Sunlight Responsive Thermochromic Window Systems...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">232</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://csrc.nist.gov/organizations/fissea/workshops/Nov2010/McDuffie_fissea-nov2010-workshop_nice-overview.pdf"> <span id="translatedtitle">Shaping the Future of Cybersecurity Education</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">... Domestic Law Enforcement and Counterintelligence Lead TBD Specialized Cybersecurity Operations <span class="hlt">NSA</span> TRACK 1 AWARENESS ...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate">2011-01-06T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">233</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://agrilifeas.tamu.edu/library/pdf/forms/ag-711.pdf"> <span id="translatedtitle">Texas A&M AgriLife Risk and Compliance AG-711 Technology Control Plan Page 1 of 7 AG-711 (07/13)</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">, the Specially Designated Nationals List, the Debarred List, the <span class="hlt">NSA</span> Nonproliferation Sanctions List, and General</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">234</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/dataexplorer/details.jsp?id=1077766"> <span id="translatedtitle">ARM's Aerosol Observing System (AOS) Data</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/dataexplorer/">DOE Data Explorer (OSTI) </a></p> <p class="result-summary">The aerosol observing system (AOS) is the primary Atmospheric Radiation Measurement (ARM) platform for in situ aerosol measurements at the surface. The principal measurements are those of the aerosol absorption and scattering coefficients as a function of the particle size and radiation wavelength. Additional measurements include those of the particle number concentration, size distribution, hygroscopic growth, and inorganic chemical composition. The AOS measures aerosol optical properties to better understand how particles interact with solar radiation and influence the earth's radiation balance. The measurements are useful for calculating parameters used in radiative forcing calculations such as the aerosol single scattering albedo, asymmetry parameter, mass scattering efficiency, and hygroscopic growth. [Copied from http://www.arm.gov/instruments/aos]</p><p>The ARM Archive at Oak Ridge National Laboratory holds aerosol data from the AOS for two of the permanent ARM sites, North Slope Alaska (<span class="hlt">NSA</span>) and Southern Great Plains (<span class="hlt">SGP</span>), as well as from mobile facilities used during specific field campaigns. The AOS has collected data since 1995.</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">235</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://daac.ornl.gov/BOREAS/boreas_photos_pages/SSA-Ops_Photos.htm"> <span id="translatedtitle">SSA Operations</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Area Operations (SSA-Ops) Area Operations (SSA-Ops) "BOREAS Ops" was located at the Snodrifters Lodge, in Candle Lake, Saskatchewan. Radiosonde balloon launch at Ops The NASA Helicopter lands at Ops A meeting at the Snodrifter's Lodge Release of a radiosonde at the SSA operations center in Candle Lake. Back to the BOREAS Photo Page Index Other Sites: <span class="hlt">NSA</span> Photos ||<span class="hlt">NSA</span>-BP Photos | <span class="hlt">NSA</span>-Fen Photos | <span class="hlt">NSA</span>-OA Photos | <span class="hlt">NSA</span>-OBS Photos | <span class="hlt">NSA</span>-OJP Photos | <span class="hlt">NSA</span>-UBS Photos | <span class="hlt">NSA</span>-YJP Photos | <span class="hlt">NSA</span>-Ops Photos SSA Photos || SSA-Airport Photos | SSA-Fen Photos | SSA-Mix Photos | SSA-OA Photos | SSA-OBS Photos | SSA-OJP Photos | SSA-YA Photos | SSA-YJP Photos | SSA-Ops Photos | ORNL DAAC Home || ORNL Home || NASA || Privacy, Security, Notices || Data Citation || Rate Us || Help | User Services - Tel: +1 (865) 241-3952 or E-mail: uso@daac.ornl.gov </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">236</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/4"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">May 22, 2008 Facility News ARM Staff Changes to Note Bookmark and Share Dr. Martin Stuefer, newest member of <span class="hlt">NSA</span> team, and his plane. Dr. Martin Stuefer, newest member of <span class="hlt">NSA</span>...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">237</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://daac.ornl.gov/BOREAS/boreas_photos_pages/BOREAS_PHOTOS.htm"> <span id="translatedtitle">BOREAS Photo Gallery</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Photo Gallery Photo Gallery These pages have been created to allow users access to a photo library of the BOREAS research sites. Click the BOREAS web page to access data from the project. Also the BOREAS historical web site provides important background information on the BOREAS project The BOREAS Study Region Northern Study Area Southern Study Area The Northern Study Area (<span class="hlt">NSA</span>) Location of the <span class="hlt">NSA</span> within Canada. (click the picture for a link to the <span class="hlt">NSA</span> website) Map of the BOREAS Northern Study Area Satellite Images of the <span class="hlt">NSA</span> Satellite image of the <span class="hlt">NSA</span> (Landsat TM July 25, 1990) Land Cover Classifcation image of the <span class="hlt">NSA</span> (August 20, 1988) Route 280 The <span class="hlt">NSA</span> landscape and Highway 391 (looking east), taken from the <span class="hlt">NSA</span>-UBS tower Typical vehicle Beaver Pond Site Fen Site Old Aspen Site </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">238</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://escholarship.org/uc/item/7qs9f70w?query=Manitoba"> <span id="translatedtitle">Direct measurement of the deep soil respiration accompanying seasonal thawing of a boreal forest soil</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">in Saskatchewan and Manitoba, Canada, J. Geophys. Res. ,Spruce site in Northern Manitoba, Canada (<span class="hlt">NSA</span>-OBS or NOBS,</p> <div class="credits"> <p class="dwt_author">Hirsch, Adam I.; Trumbore, Susan E.; Goulden, Michael L.</p> <p class="dwt_publisher"></p> <p class="publishDate">2002-01-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">239</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://csrc.nist.gov/cyberframework/rfi_comments/040813_peregrine_technical_solutions.pdf"> <span id="translatedtitle">CORPORATE CAPABILITIES</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">... <span class="hlt">NSA</span> sponsored IA programs and curriculum. ... comprehensive critical infrastructure curricula or graduate ... Nascent master's curriculums are underway ...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate">2013-04-09T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">240</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00101.pdf"> <span id="translatedtitle">Slide 1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">a Mesoscale Convective System Sampled During <span class="hlt">TWP</span>-ICE: Analysis via Water Budget Equations Jasmine Cetrone and Robert Houze University of Washington Introduction This study computes...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_11");' href="#" title="Previous Page"> <img id="PreviousPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.previous.18x20.png" alt="Previous Page" /></a> <span id="PageLinks" class="pageLinks"> <span> <a onClick='return showDiv("page_1");' href="#">1</a> <a onClick='return showDiv("page_2");' href="#">2</a> <a onClick='return showDiv("page_3");' href="#">3</a> <a 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</div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">242</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/highlights/RMjc=/view"> <span id="translatedtitle">Research Highlight</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">(<span class="hlt">TWP</span>) site at Manus, Papua New Guinea. Drought conditions and population pressures in Indonesia and surrounding areas of the Tropical West Pacific sparked massive biomass burning...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">243</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00177.pdf"> <span id="translatedtitle">Microsoft PowerPoint - DAR_Monsoon_CNL2007c.ppt</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">March 2007 ARM Science Team Meeting Relating the <span class="hlt">TWP</span>-ICE Period to Darwin Climatology Chuck Long and Jim Mather, Pacific Northwest National Laboratory Peter May, Australian Bureau...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">244</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/highlights/RMTA2/view"> <span id="translatedtitle">Research Highlight</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Importance of Small Ice Crystals to Cirrus Properties: Observations from <span class="hlt">TWP</span>-ICE Download a printable PDF Submitter: McFarquhar, G., University of Illinois, Urbana Area of...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">245</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf14/extended_abs/vogelmann-am.pdf"> <span id="translatedtitle">A Lagrangian Interpretation of 3D Tropical Cloud Structure: ...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">the distributions requires further investigation, the implications are that <span class="hlt">TWP</span>-Microbase retrieval would provide information about the tropical cloud water content for 2...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">246</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/sites/prod/files/CX-008503.pdf"> <span id="translatedtitle">NETL F 451.1/1-1, Categorical Exclusion Designation Form</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">Chris Johnson Orion <span class="hlt">Twp</span>, Michigan Development of Advanced High Energy Batteries for EV Applications Test battery cells, incorporate into packs and test, and modeling....</p> <div class="credits"> <p class="dwt_author"></p> <p 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<p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">248</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/campaigns/aaf2007clasic"> <span id="translatedtitle">ARM - Field Campaign - Cloud LAnd Surface Interaction Campaign (CLASIC)</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">govCampaignsCloud LAnd Surface Interaction Campaign (CLASIC) govCampaignsCloud LAnd Surface Interaction Campaign (CLASIC) Campaign Links CLASIC Website Related Campaigns CLASIC - SAM Support 2007.06.09, DeVore, <span class="hlt">SGP</span> CLASIC - 9.4 GHz Phase Array Radar 2007.06.08, Kollias, <span class="hlt">SGP</span> CLASIC - Southern Great Plains Aerosol Evolution Study (SGPAES) 2007.06.08, Collins, <span class="hlt">SGP</span> CLASIC - Land Surface 2007.06.01, Jackson, <span class="hlt">SGP</span> CLASIC - Radiosonde Campaign 2007.06.01, Orr, <span class="hlt">SGP</span> CLASIC - <span class="hlt">SGP</span> Particle Phase Experiment 2007.06.01, Martin, <span class="hlt">SGP</span> CLASIC - Land-Cloud Coupled Data Assimilation System 2007.06.01, Jackson, <span class="hlt">SGP</span> Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Campaign : Cloud LAnd Surface Interaction Campaign (CLASIC) 2007.06.01 - 2007.06.30 Website : http://acrf-campaign.arm.gov/clasic/ Lead Scientist : Mark Miller </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">249</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/data/datastreams/915rwpprecipcon"> <span id="translatedtitle">ARM - Datastreams - 915rwpprecipcon</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Auxiliary) <span class="hlt">SGP</span> S07 Browse Data Supplemental 7, Lamont, OK <span class="hlt">SGP</span> S08 Browse Data Supplemental 8, Lamont, OK ARM Mobile Facility PVC M1 Browse Data Highland Center, Cape Cod MA; AMF 1...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">250</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.evs.anl.gov/user-facilities/sgp/"> <span id="translatedtitle">The Southern Great Plains Site: A Climate Observatory in Oklahoma</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">other facilities throughout the <span class="hlt">SGP</span> site. The 60-ft meteorological tower rises from a canola field at the <span class="hlt">SGP</span> central facility in June 2011. The 60-ft meteorological tower rises...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">251</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00099.pdf"> <span id="translatedtitle">PowerPoint Presentation</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary"><span class="hlt">TWP</span> <span class="hlt">TWP</span> Storm Types <span class="hlt">TWP</span> Storm Types Fig. 1. ARM <span class="hlt">TWP</span> sites experience different convective clouds within the <span class="hlt">TWP</span>: (1) ITCZ, (2) SPCZ, (3) Island convection, and (4) Coastal convection. ARM sites: D = Darwin, M = Manus, N = Nauru). Plot color scheme: yellow is cold, blue is warm. 1 2 3 4 M M N N D D 6 December, 2005, 5:30 GMT 6 December, 2005, 5:30 GMT 1. OVERVIEW 1. OVERVIEW A. Previous Work A. Previous Work Tracked clouds with geostationary satellite data to determine the context of the cloud state observed at the ARM Sites, such as the cloud's life-cycle stage and its representativeness of the region. B. Goal B. Goal Expanding classification system for: * Cloud regime classification * Convective regime classification * Subsequent tracking of features' paths and </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">252</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/extended_abs/teske_jj.pdf"> <span id="translatedtitle">Microsoft Word - Teske-JJ.doc</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Analysis of the Corrective Maintenance Analysis of the Corrective Maintenance Records of the ARM <span class="hlt">SGP</span> CART J. J. Teske Aeromet Corporation Tulsa, Oklahoma J. C. Liljegren and D. L. Sisterson Environmental Research Division Argonne National Laboratory Argonne, Illinois Introduction The primary responsibility of Southern Great Plains (<span class="hlt">SGP</span>) Site Operations is to operate and maintain the Atmospheric Radiation Measurement (ARM) instruments at the <span class="hlt">SGP</span> Cloud and Radiation Testbed (CART) facilities. Since 1992, <span class="hlt">SGP</span> Site Operations has maintained detailed corrective maintenance records for the ARM <span class="hlt">SGP</span> instruments as part of the <span class="hlt">SGP</span> Operations and Maintenance Information System (OMIS). These records are available online at http://www.ops.<span class="hlt">sgp</span>.arm.gov. We analyzed these records back to 1995. They reveal maintenance trends that vary by instrument type, location, and year. </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">253</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.cs.indiana.edu/~minaxi/pubs/dimva09.pdf"> <span id="translatedtitle">A Case Study on Asprox Infection Dynamics Youngsang Shin1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">by Holz et al in [13]: FA = NA/nA average single (1) FNS = NNS/nNS average single (2) f<span class="hlt">NSA</span> = NNSA /n<span class="hlt">NSA</span> of NS records returned for a single DNS resolution. NNSA is the number of unique A records, that is, IP addresses returned in all DNS resolutions for a DNS server. n<span class="hlt">NSA</span> average single the average number</p> <div class="credits"> <p class="dwt_author">Gupta, Minaxi</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">254</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/poster_abs/P00057"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Measurements at the DOE ARM <span class="hlt">NSA</span> Site Dong, X. and Mace, G.G., University of Utah Eleventh Atmospheric Radiation Measurement (ARM) Science Team Meeting The Arctic plays...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">255</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://csrc.nist.gov/nice/training.htm"> <span id="translatedtitle">The National Initiative for Cybersecurity Education (NICE)</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">... and Professional Development is led by the ... and Counterintelligence (Co-Leads: DOD/DC3 ... 4: Specialized Cybersecurity Operations (Lead: <span class="hlt">NSA</span>). ...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate">2013-07-09T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">256</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://daac.ornl.gov/BOREAS/boreas_photos_pages/SSA-Mix_Photos.htm"> <span id="translatedtitle">SSA Mixed Canopy Site</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Mixed Canopy Site (SSA-Mix) Mixed Canopy Site (SSA-Mix) The TE canopy tower The mixed trees Terrestrial Ecology canopy access tower at the SSA mixed coniferous/deciduous site. A picture taken looking down from the TE canopy access tower at the SSA mixed auxiliary site, showing the aspen and spruce canopies. Back to the BOREAS Photo Page Index Other Sites: <span class="hlt">NSA</span> Photos ||<span class="hlt">NSA</span>-BP Photos | <span class="hlt">NSA</span>-Fen Photos | <span class="hlt">NSA</span>-OA Photos | <span class="hlt">NSA</span>-OBS Photos | <span class="hlt">NSA</span>-OJP Photos | <span class="hlt">NSA</span>-UBS Photos | <span class="hlt">NSA</span>-YJP Photos | <span class="hlt">NSA</span>-Ops Photos SSA Photos || SSA-Airport Photos | SSA-Fen Photos | SSA-Mix Photos | SSA-OA Photos | SSA-OBS Photos | SSA-OJP Photos | SSA-YA Photos | SSA-YJP Photos | SSA-Ops Photos | ORNL DAAC Home || ORNL Home || NASA || Privacy, Security, Notices || Data Citation || Rate Us || Help | User Services - Tel: +1 (865) 241-3952 or E-mail: uso@daac.ornl.gov </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">257</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/products/eionline"> <span id="translatedtitle">USDOE, Office of Scientific and Technical Information</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/home/">Office of Scientific and Technical Information (OSTI)</a></p> <p class="result-summary">Energy Information Online Energy Science and Technology Database (EDB) and Nuclear Science Abstracts (<span class="hlt">NSA</span>) The Department of Energy's legacy bibliographic databases, Energy Science...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">258</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.nist.gov/mml/msed/thermodynamics_kinetics/upload/MGI-Overview-Digest-for-PCO.pdf"> <span id="translatedtitle">NIST and The Materials Genome Initiative</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">... the Materials Genome Ini(a(ve formed (NIST, DOE, DOD, NSF, NASA, NIH, USGS, NNSA, DARPA, <span class="hlt">NSA</span>, OMB) 6/12: MGI White House Kickoff Event ...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate">2013-07-02T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">259</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/cio/office-chief-information-officer/services/incident-management"> <span id="translatedtitle">Incident Management | Department of Energy</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">Virus Pages Sophos Virus Info Page Symantec Trend Micro Virus Encyclopedia Virus Bulletin Home Page Cyber Security Sites AUSCERT FIRST <span class="hlt">NSA</span> (National Security Agency) NVD (National...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">260</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://escholarship.org/uc/item/66h3f5pm?query=Manitoba"> <span id="translatedtitle">The surface CO2 gradient and pore-space storage flux in a high-porosity litter layer</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">at a site in northern Manitoba, Canada. The profile data,Spruce site in northern Manitoba, Canada (<span class="hlt">NSA</span>- OBS or NOBS,</p> <div class="credits"> <p class="dwt_author">HIRSCH, ADAM I.; TRUMBORE, SUSAN E.; GOULDEN, MICHAEL L.</p> <p class="dwt_publisher"></p> <p class="publishDate">2004-01-01T23:59:59.000Z</p> </div> </div> </div> </div> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_12");' href="#" title="Previous Page"> <img id="PreviousPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.previous.18x20.png" alt="Previous Page" /></a> <span id="PageLinks" class="pageLinks"> 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Those that will be serving one-year terms will be Pauline Bowen, HHS, Vicki Jordan, <span class="hlt">NSA</span>, Sharon Kavanaugh, HCFA, and Phil Sibert, DOE. ...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">262</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/60th/1970/index"> <span id="translatedtitle">USDOE, Office of Scientific and Technical Information</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/home/">Office of Scientific and Technical Information (OSTI)</a></p> <p class="result-summary">Section 1973: MainFrame TapeBackup 1973: Photolab 1973: Typesetting 1973: VAX Computers 1974: Nuclear Science Abstracts (<span class="hlt">NSA</span>) 1975: Graphic Arts 1975: Editing 1979: Manager...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">263</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.nersc.gov/...requirements-reviews/target-2014/FES/fes-case-study-worksheets/charlson-kim/"> <span id="translatedtitle">NERSC/DOE FES Requirements Workshop Worksheet - Charlson Kim</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Charlson Kim Participating Organizations U. Washington, U. Wisconsin-Madison, Utah State, NRL Funding Agencies DOE SC DOE <span class="hlt">NSA</span> NSF NOAA NIH Other: 2. Project Summary &...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">264</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://csrc.nist.gov/organizations/fissea/educator-year/04nomination.html"> <span id="translatedtitle">2004 Educator of the Year Award - Dr. Gail-Joon Ahn</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">... Ahn. Dr. Ahn's students are working in many federal agencies including <span class="hlt">NSA</span>, NRL, VA, GAO, DIA, US Navy, and ORNL. Dr ...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">265</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.nist.gov/itl/iad/talukder.cfm"> <span id="translatedtitle">Ashit Talukder</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">... The programs that he leads at IAD involves collaborations within NIST, and with many federal agencies including DARPA, IARPA, <span class="hlt">NSA</span>, FBI, DoD ...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate">2013-02-07T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">266</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/sites/nsa/fsp_auth"> <span id="translatedtitle">ARM - Firearm Training and Authorization List</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">AlaskaFirearm Training and Authorization List <span class="hlt">NSA</span> Related Links Facilities and Instruments Barrow Atqasuk ES&H Guidance Statement Operations Science Field Campaigns Visiting the...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">267</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.nist.gov/nvlap/upload/NVLAP_News_Spring_Summer_2013.pdf"> <span id="translatedtitle">Farewell Betty Ann Sandoval</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">... wrote rules and regulations for the safe use of nuclear materials and ... of Standards and Technology (NIST), and the National Security Agency (<span class="hlt">NSA</span> ...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate">2013-07-31T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">268</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/extended_abs/bahrmann_cp.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary"><span class="hlt">SGP</span> Site Scientist Team and ARM Data Quality Office <span class="hlt">SGP</span> Site Scientist Team and ARM Data Quality Office <span class="hlt">SGP</span> Data Quality Assessment Activities: A New Approach C. P. Bahrmann, R. A. Peppler, K. Sonntag, and A. Dean Cooperative Institute for Mesoscale Meteorological Studies University of Oklahoma Norman, Oklahoma Introduction A primary task of the Site Scientist Team (SST) of the Southern Great Plains (<span class="hlt">SGP</span>) Cloud and Radiation Testbed (CART) site is to analyze and assess the quality of various <span class="hlt">SGP</span> data streams. The opening of the Atmospheric Radiation Measurement (ARM) Program Data Quality Office (DQO) allowed for a cooperative effort between the <span class="hlt">SGP</span> SST, Instrument Mentors (IM), and DQO. This approach led to the development of new tools for assessing data quality, reporting problems, and issuing </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">269</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/BAMS-D-11-00137.1"> <span id="translatedtitle">ARM Research In The Equatorial Western Pacific: A Decade And Counting</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">The tropical western Pacific (<span class="hlt">TWP</span>) is an important climatic region. Strong solar heating, warm sea surface temperatures, and the annual progression of the intertropical convergence zone (ITCZ) across this region generate abundant convective systems, which ...</p> <div class="credits"> <p class="dwt_author">C. N. Long; S. A. McFarlane; A. Del Genio; P. Minnis; T. P. Ackerman; J. Mather; J. Comstock; G. G. Mace; M. Jensen; C. Jakob</p> <p class="dwt_publisher"></p> <p class="publishDate">2013-05-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">270</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/BAMS-89-5-629"> <span id="translatedtitle">The Tropical Warm Pool International Cloud Experiment</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">A comprehensive dataset describing tropical cloud systems and their environmental setting and impacts has been collected during the Tropical Warm Pool International Cloud Experiment (<span class="hlt">TWP</span>-ICE) and Aerosol and Chemical Transport in Tropical ...</p> <div class="credits"> <p class="dwt_author">Peter T. May; James H. Mather; Geraint Vaughan; Keith N. Bower; Christian Jakob; Greg M. McFarquhar; Gerald G. Mace</p> <p class="dwt_publisher"></p> <p class="publishDate">2008-05-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">271</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/fact-sheets/docs/doe-sc-arm-11-010.pdf"> <span id="translatedtitle">FACT SHEET U.S. Department of Energy Tropical Western...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Pool" The <span class="hlt">TWP</span> locale spans an area roughly between 10N to 10S of the equator from Indonesia to the International Date Line. This region of the world plays a large role in the...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">272</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/brochures/docs/doe-sc-arm-p-05-010.pdf"> <span id="translatedtitle">Visiting Scientists and Researchers</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Barrow. Tropical Western Pacific The <span class="hlt">TWP</span> site includes an area at the equator near Indonesia. This region of the world plays a large role in the interan- nual variability...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">273</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf08/extended_abs/parsons_db.pdf"> <span id="translatedtitle">parsons-98.pdf</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">the very dry air in the troposphere over the <span class="hlt">TWP</span> does not come about from strong subsidence of tropical air, as perhaps generally thought, during the suppressed phases of the...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">274</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/JAMC-D-12-0189.1"> <span id="translatedtitle">A Climatology of Surface Cloud Radiative Effects at the ARM Tropical Western Pacific Sites</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">Cloud radiative effects on surface downwelling fluxes are investigated using datasets from the Atmospheric Radiation Measurement Program (ARM) sites in the tropical western Pacific Ocean (<span class="hlt">TWP</span>) region. The Nauru Island (Republic of Nauru) and ...</p> <div class="credits"> <p class="dwt_author">Sally A. McFarlane; Charles N. Long; Julia Flaherty</p> <p class="dwt_publisher"></p> <p class="publishDate">2013-04-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">275</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/meetings/2009/presentations/0331/16_Zeng.pdf"> <span id="translatedtitle">Modeling the Effect of Ice Nuclei on ARM Clouds</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Upper-Tropospheric Ice Water Content in <span class="hlt">TWP</span>-ICE Xiping Zeng, Wei-Kuo Tao, Minghua Zhang, and Shaochen Xie March 31, 2009 Papers Published Recently * Zeng, X., W.-K. Tao, M. Zhang,...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">276</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00018.pdf"> <span id="translatedtitle">Slide 1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">3-D Cloud Ice Water Features Determined by Combining Satellite and Surface Measurements during <span class="hlt">TWP</span>-ICE G. Liu and E.-K. Seo, Florida State University Objectives Large-scale...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">277</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00041.pdf"> <span id="translatedtitle">Microsoft PowerPoint - McFarquhar_2007.ppt</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Small Ice Crystals during <span class="hlt">TWP</span>-ICE Greg M. McFarquhar 1 , Junshik Um 1 , Matt Freer 1 , Darrel Baumgardner 2 , Gregory L. Kok 3 and Gerald G. Mace 4 1 Department of Atmospheric...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">278</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/abs/10.1175/JCLI3326.1?prevSearch=%5BFulltext%3A+LANL%5D&searchHistoryKey="> <span id="translatedtitle">The Radiative, Cloud, and Thermodynamic Properties of the Major Tropical Western Pacific Cloud Regimes</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">This study investigates the radiative, cloud, and thermodynamic characteristics of the atmosphere separated into objectively defined cloud regimes in the tropical western Pacific (<span class="hlt">TWP</span>). A cluster analysis is applied to 2 yr of daytime-only data ...</p> <div class="credits"> <p class="dwt_author">Christian Jakob; George Tselioudis; Timothy Hume</p> <p class="dwt_publisher"></p> <p class="publishDate">2005-04-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">279</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/data/post/22701"> <span id="translatedtitle">ARM - Data Announcements Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">August 29, 2013 Data Announcements New Data Available for Precipitation Value-Added Product A spatial plot of rainfall intensity (mmh) centered on the Manus (<span class="hlt">TWP</span>-C1) central...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">280</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/.../prod/files/2013/11/f4/webcast_20100805_achieving_total_employee_engagement.pdf"> <span id="translatedtitle">Achieving Total Employee Engagement in Energy Efficiency</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">23% 77% Bowling Green 61% 30% 91% CAMI n a n a n a Fairfax Assy & Contig 49% 21% 70% Flint Assy 49% 19% 68% Fort Wayne 58% 21% 79% Hamtramck 63% 37% 100% Lansing 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<center><strong>Note: This page contains sample records for the topic "nsa sgp twp" from the National Library of Energy<sup>Beta</sup> (NLE<sup>Beta</sup>).<br> While these samples are representative of the content of NLE<sup>Beta</sup>,<br> they are not comprehensive nor are they the most current set.<br> We encourage you to perform a <a href="http://www.osti.gov/nle">real-time search of NLE<sup>Beta</sup></a><br> to obtain the most current and comprehensive results.</strong></center><p><br></p> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_14");' href="#" title="Previous Page"> 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</div> <a href="http://www.osti.gov/nle/topicpages">Index</a> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">281</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/sites/prod/files/CX-008333.pdf"> <span id="translatedtitle">NETL F 451.1/1-1, Categorical Exclusion Designation Form</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">NA NETL ORD FE RES-URS ORD 2012 - 2017 John Baltrus NETL: South Park <span class="hlt">Twp</span>, PA (B83-341) Surface Analysis Laboratory (Site Relocation) The project houses an x-ray photoelectron...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">282</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/sites/prod/files/CX-008961.pdf"> <span id="translatedtitle">NETL F 451.1/1-1, Categorical Exclusion Designation Form</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">Not Yet Assigned NETLSOD FE SOD 2012 9 months Colleen Butcher (COR) NETL: South Park <span class="hlt">Twp</span>., PA Pittsburgh Guard Shack Replacement The guard shacks on the R&D plateau and the 920...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">283</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/sites/prod/files/CX-004703.pdf"> <span id="translatedtitle">NETL F 451.1-1/1 Categorical Exclusion (CX) Designation Form</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">NA Not yet awarded. DOENETL NA NETLSODS 2010 Thomas W. Snyder 120 Days from NTP NETL South Park <span class="hlt">Twp</span>, Allegheny Cty, PA Building 74 Exterior Brick Work Repair deteriorated...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">284</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/sites/prod/files/CX-007934.pdf"> <span id="translatedtitle">NETL F 451.1/1-1, Categorical Exclusion Designation Form</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">0192 NETL ORD FE ORD 2012 June 2011 to June 2016 Dr. Bret Howard NETL: South Park <span class="hlt">Twp</span>, PA (94-411) UHV Materials Chemistry Laboratory Ultra-high vacuum-based research addressing...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">285</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/sites/prod/files/CX-007482.pdf"> <span id="translatedtitle">NETL F 451.1/1-1, Categorical Exclusion Designation Form</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">DT0003144 NETL SOD FE Eagle Design SOD 2012 210 days David A. Schmidt NETL: South Park <span class="hlt">Twp</span>, PA B94 Hazardous Gas Alarms Providing gas alarm monitoring sensing systems into Labs...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">286</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/sites/prod/files/2013/04/f0/CX-009466.pdf"> <span id="translatedtitle">NETL F 451.1/1-1, Categorical Exclusion Designation Form</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">0198 DOE NETL FE ORDCSSD Continuous Chris Matranga South Park <span class="hlt">Twp</span>, PA (B-83 Rm. 332) Pittsburgh Spectroscopy and Electrochemistry Lab A general-use laboratory for fuel, energy,...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">287</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/sites/prod/files/CX-005636.pdf"> <span id="translatedtitle">NETL F 451.1-1/1 Categorical Exclusion (CX) Designation Form</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">DE-FE0011994 Modification 3 ESS&H Division 2011 Allen Lichvar 1 May 2011 - 31 Oct 2011 NETL Pittsburgh, South Park <span class="hlt">Twp</span>, PA ReplacementInstallation of Physical Access Control...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">288</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.econ.iastate.edu/tesfatsi/ComplexityEconomics.WBrianArthur.SFIWP2013.pdf"> <span id="translatedtitle">Complexity Economics: A Different Framework</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">in the gross profits References Aghion P, Howitt P (1992) A model of growth through creative destruction IV van Dijk <span class="hlt">TWP</span> (1994) The limits of patent protection. Essays on the Economics of Intellectual</p> <div class="credits"> <p class="dwt_author">Tesfatsion, Leigh</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">289</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/campaigns/twp2006twp-ice"> <span id="translatedtitle">ARM - Field Campaign - Tropical Warm Pool - International Cloud...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">the US DOE ARM project, the Bureau of Meteorology, NASA, the European Commission DG RTD-1.2 and several United States, Australian, Canadian and European Universities. <span class="hlt">TWP</span>-ICE...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">290</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/sites/prod/files/2013/09/f2/CX-010605.pdf"> <span id="translatedtitle">NETL F 451.1/1-1, Categorical Exclusion Designation Form</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">Not Assigned Yet Not Procured Yet FE OIOSOD 2014 Colleen Butcher NETL, South Park <span class="hlt">Twp</span>, PA Building 58 Third Floor Mezzanine Enclosure Enclose the third floor mezzanine of B 58....</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">291</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/1038"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">rainfall rate and for improving these parameterizations in models that predict weather. Between May and June, the ARM Southern Great Plains (<span class="hlt">SGP</span>) site is hosting a joint...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">292</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/highlights/RNTAw/view"> <span id="translatedtitle">Research Highlight</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Plains (<span class="hlt">SGP</span>) site. The team included a parameterization to represent irrigation in the Noah land surface model applied in WRF, and conducted a series of simulations with and...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">293</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/182"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">UNIX and Windows system management, network management, and software and hardware troubleshooting. Keith's initial tasks will be to learn the systems architectures at the <span class="hlt">SGP</span> with...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">294</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/extended_abs/feltz_wf.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">U.S. Department of Energy (DOE) Atmospheric Radiation Measurement (ARM) sites. The AERI plus retrievals from the Southern Great Plains (<span class="hlt">SGP</span>) site will show improvement in the...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">295</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf09/extended_abs/anderberg_mhl.pdf"> <span id="translatedtitle">anderberg-99.PDF</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Renewable Energy Laboratory (NREL) performs a quality assessment of the data from 22 Solar Infrared Radiation Stations (SIRS) in the Southern Great Plains (<span class="hlt">SGP</span>) on a...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">296</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/13403"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">approximately 22,500 square kilometers, or the approximate area of a modern climate model grid cell. Centered around the <span class="hlt">SGP</span> Central Facility, these extended facilities are...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">297</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/annual-reports/docs/doe-sc-arm-11-024.pdf"> <span id="translatedtitle">DOE/SC-ARM-11-024 ARM Climate Research Facility ANNUAL REPORT...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">2011 Recovery Act HIGHLIGHTS October 2010 * Doppler lidars tested at the Atmospheric Radiation Measurement (ARM) Climate Research Facility's Southern Great Plains (<span class="hlt">SGP</span>) site. *...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">298</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf09/extended_abs/guichard2_f.pdf"> <span id="translatedtitle">guichard(2)-99.pdf</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Ninth ARM Science Team Meeting Proceedings, San Antonio, Texas, March 22-26, 1999 1 Evaluating Mesoscale Model Predictions and Parameterizations Against <span class="hlt">SGP</span> ARM Data on a Seasonal...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">299</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/tech_reports/doe-sc-arm-tr-102.pdf"> <span id="translatedtitle">DOE/SC-ARM-TR-102 Sonde Adjust Value-Added Product Technical...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">... 14 Figures 1 The original and corrected relative humidity profile for Vaisala RS-92 radiosondes launched at the <span class="hlt">SGP</span> Central Facility on May 12,...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">300</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/instruments/twr"> <span id="translatedtitle">ARM - Instrument - twr</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">are listed in section 7, Instrument Details, although only the TemperatureRelative HumidityVapor Pressure (TRHVP) measurements made on the <span class="hlt">SGP</span> CF tower are described in...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p 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class="resultNumber element">301</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/poster_abs/P00143"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Subgrid-Scale Vertical Transport of Moisture and Energy Over the ARM <span class="hlt">SGP</span>: Analysis of Measurements and Parameterizations in Cumulus Convection Schemes Zhang, M.H., State University...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">302</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/highlights/RMjkz/view"> <span id="translatedtitle">Research Highlight</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Trends in Downwelling Longwave Radiation over <span class="hlt">SGP</span> Download a printable PDF Submitter: Gero, J., University of Wisconsin Turner, D. D., National Oceanic and Atmospheric...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">303</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf03/extended_abs/sisterson_dl.pdf"> <span id="translatedtitle">Instrumentation for Southem Great Plains D. L. Sisterson and...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">counties are outlined. 318 Instrumentation for Southern Great Plains Table 1. Dates of installations of Instrumentation, side data system versions, and facilities at the <span class="hlt">SGP</span>...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">304</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/meetings/2009/presentations/0330/7_Xie.pdf"> <span id="translatedtitle">SCM Working Group</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Atmospheric Radiation Measurement How Do the Variational Analysis and SCMsCRMs Respond to a Reduced ARM <span class="hlt">SGP</span> Network? Shaocheng Xie Lawrence Livermore National Laboratory...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">305</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf13/extended_abs/shi-y.pdf"> <span id="translatedtitle">Preliminary Analysis of Surface Radiation Measurement Data Quality...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">primary radiation flux measurements at the <span class="hlt">SGP</span> extended facilities are obtained from the Solar Infrared Radiation Station (SIRS). In this study, we examine the radiation...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">306</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf06/extended_abs/splitt_me.pdf"> <span id="translatedtitle">Section 69</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">C comparison of Solar and Infrared Observation Station (SIROS) hemispheric broadband solar observations at Atmospheric Radiation Measurement (ARM) <span class="hlt">SGP</span> Extended Facilities...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">307</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://escholarship.org/uc/item/9vf428rc?query=Geothermal"> <span id="translatedtitle">A PLAUSIBLE TWO-DIMENSIONAL VERTICAL MODEL OF THE EAST MESA GEOTHERMAL FIELD, CALIFORNIA, U.S.A</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">~:::. -:: .. ::_ Geothermal Reservoir , <span class="hlt">SGP</span> .. ~TR~/+ 0,CUl'{ER of the p,. l'1~esa Geothermal Anomaly, Imperial 58,convection in an unconfined geothermal reservoir, IGPP 72-</p> <div class="credits"> <p class="dwt_author">Goyal, K.P.</p> <p class="dwt_publisher"></p> <p class="publishDate">2013-01-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">308</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/18720"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Kim; Doug Sisterson, <span class="hlt">SGP</span> site manager; Dr. Seungsook Shin; and Dr. Kwan-Young Chung. In Korea, typhoons and heavy rainfallsnowfall often result in serious socio-economic...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">309</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf16/poster_abs/P00106"> <span id="translatedtitle">Measuring the Raindrop Size Distribution, ARM's Efforts at Darwin...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Measuring the Raindrop Size Distribution, ARM's Efforts at Darwin and <span class="hlt">SGP</span> Bartholomew, Mary Jane Brookhaven National Laboratory Category: Instruments ARM has purchased two impact...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">310</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf15/poster_abs/P00191"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents: Spectral...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">over the ARM <span class="hlt">SGP</span> area from multi-year satellite observations Trishchenko, Alexander Canada Centre for Remote Sensing Luo, Yi Canada Centre for Remote Sensing Li, Zhanqing...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">311</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf19/poster/P00022.pdf"> <span id="translatedtitle">Microsoft PowerPoint - arm_stm09-poster_matrosov.ppt</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Precipitation Parameters above the <span class="hlt">SGP</span> site during spring-summ Sergey Y. Matrosov Cooperative Institute for Research in Environmental Sciences, University of Colorado and NOAA...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">312</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf13/extended_abs/kogan-zn.pdf"> <span id="translatedtitle">The Effect of Precipitation on Variability of Low Stratiform...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Low Stratiform Clouds Over ARM <span class="hlt">SGP</span> Site Z. N. Kogan, D. B. Mechem, and Y. L. Kogan Cooperative Institute for Mesoscale Metorological Studies University of Oklahoma Norman,...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">313</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf09/extended_abs/spinhirne_jd.pdf"> <span id="translatedtitle">spinhirne-99.PDF</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Retrieval Comparison During the <span class="hlt">SGP</span> Summer '98 IOP From Multiple Lidar Probing J. D. Spinhirne National Aeronautics and Space Administration Goddard Space Flight Center Greenbelt,...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">314</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://daac.ornl.gov/BOREAS/boreas_photos_pages/NSA-YJP_Photos.htm"> <span id="translatedtitle">Young Jack Pine Site</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary"><span class="hlt">NSA</span>-YJP) The hut, tent, and dirt road from the flux tower The sun photometer on top of the hut The bottom of the YJP flux tower <span class="hlt">NSA</span>-YJP taken at a low sun angle to show the subtle...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">315</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/1527"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Satellite Service Conserves Cash Satellite Service Conserves Cash Bookmark and Share In April, operations personnel completed a series of cost-saving data communication changes at the ARM Climate Research Facility Southern Great Plains (<span class="hlt">SGP</span>) locale. The T-1 telephone lines at the four <span class="hlt">SGP</span> boundary facilities were replaced with satellite dish technology. This change still allows large data sets to be transferred at acceptable bandwidth but at substantial savings. Inexpensive satellite services now meet data transmission needs at the <span class="hlt">SGP</span> boundary facilities. Inexpensive satellite services now meet data transmission needs at the <span class="hlt">SGP</span> boundary facilities. Huge amounts of data are collected daily by <span class="hlt">SGP</span> site instruments. These data must be transmitted rapidly and reliably from remote measurement </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">316</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf19/poster/P00137.pdf"> <span id="translatedtitle">Orr 2009 ARM STM poster2.ppt</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Status: Design, testing and implementation has been begun at <span class="hlt">SGP</span> Status: Design, testing and implementation has been begun at <span class="hlt">SGP</span> A U.S. Department of Energy laboratory managed by UChicago-Argonne, LLC Accomplishments and Status of <span class="hlt">SGP</span> During 2008 Brad W. Orr 1 Dan J. Rusk 2 John Schatz 2 David Breedlove 2 Richard Eagan 1 1 Argonne National Laboratory, Argonne, IL 2 ACRF/<span class="hlt">SGP</span>, Cherokee Nation Distributors, Stilwell, OK INSTRUMENTS GENERAL STATISTICS * Instrument Availability - Averaged over 95% during 2008. * Electronic Repair Lab - $20,000 in savings * Calibrations - Over 140 instruments calibrated * Guest Instruments Supported - 40 * Site visitors - Over 100 visits by scientists and guests at the Central Facility. * Field Campaigns - 18 Campaigns supported last year. Acknowledgments We would like to thank the entire <span class="hlt">SGP</span> staff for another year of excellence and for their continued support of all aspects of operations. This </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">317</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/9436"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">15, 2010 [Facility News] 15, 2010 [Facility News] Water Vapor Network at <span class="hlt">SGP</span> Site Goes Offline Bookmark and Share Each of the 24 solar-powered GPS stations streamed data via a wireless network to the <span class="hlt">SGP</span> Central Facility for data collection and storage. Each of the 24 solar-powered GPS stations streamed data via a wireless network to the <span class="hlt">SGP</span> Central Facility for data collection and storage. After nearly eleven years, the Single Frequency GPS Water Vapor Network field campaign at the ARM Southern Great Plains (<span class="hlt">SGP</span>) site came to a close on July 1, 2010. Installed between 1999 and 2000, this network consisted of 24 GPS stations operating within an 8-kilometer radius around the <span class="hlt">SGP</span> Central Facility near Lamont, Oklahoma. Developed to function as a single instrument, the network simultaneously measured "slant water vapor" in </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">318</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/872"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">February 28, 2006 [Facility News] February 28, 2006 [Facility News] Network of Infrared Thermometers Nearly Complete at <span class="hlt">SGP</span> Bookmark and Share Red dots indicate extended facilities at <span class="hlt">SGP</span> with the new IRTs installed; green dots indicate future installations. Red dots indicate extended facilities at <span class="hlt">SGP</span> with the new IRTs installed; green dots indicate future installations. As reported in April 2005, a network of infrared thermometers (IRT) is being installed throughout the ARM Southern Great Plains (<span class="hlt">SGP</span>) site for the purpose of measuring cloud base temperature and inferring cloud base height across the domain. These measurements will enhance existing <span class="hlt">SGP</span> surface and satellite cloud measurements to help scientists improve their calculations of heating rate profiles on the scale of global climate models. The first </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">319</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/sites/nsa/docs/nsa_fsp.pdf"> <span id="translatedtitle">ACTIVITY SPECIFIC FIREARMS SAFETY PLAN FOR </span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Atmospheric Radiation Measurement Climate Research Facility/ Atmospheric Radiation Measurement Climate Research Facility/ North Slope of Alaska/Adjacent Arctic Ocean (ACRF/<span class="hlt">NSA</span>/AAO) Activity Specific Firearm Safety Plan for ACRF/North Slope of Alaska Sandia National Laboratories Department 6383, Energy, Climate & Atmospheric Management ACRF/<span class="hlt">NSA</span>/AAO Revision 14 Activity Specific Firearm Safety Plan for June 2010 ACRF/North Slope of Alaska Signature Page This safety plan is approved by the undersigned and includes the firearm and ammunition storage practices described in this document. Mark D Ivey ACRF/<span class="hlt">NSA</span>/AAO Site Manager _________________________________Date: ______ Mark D Ivey Department 06339 Manager _________________________________Date: _______ Michael L Heister SNL Safety Engineer _________________________________Date:________ </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">320</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/campaigns/aaf2008isdac"> <span id="translatedtitle">ARM - Field Campaign - Indirect and Semi-Direct Aerosol Campaign (ISDAC)</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">govCampaignsIndirect and Semi-Direct Aerosol Campaign (ISDAC) govCampaignsIndirect and Semi-Direct Aerosol Campaign (ISDAC) Campaign Links ISDAC Website Related Campaigns Parameterization of Extinction Coefficient in Ice and Mixed-Phase Arctic Clouds During ISDAC 2010.10.01, Korolev, AAF ISDAC - Second Year Supplemental Surface Spectral Irradiance Measurements 2009.04.07, Lubin, <span class="hlt">NSA</span> ISDAC - NASA ARCTAS Coordination with ARM 2008.04.01, Ferrare, <span class="hlt">NSA</span> ISDAC / RISCAM - Humidified Tandem Differential Mobility Analyzer (HTDMA) 2008.04.01, Collins, <span class="hlt">NSA</span> ISDAC - Hemispheric Flux Spectroradiometer 2008.03.31, Lubin, <span class="hlt">NSA</span> Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. 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class="Icon" src="http://www.osti.gov/nlesearch/images/icon.last.18x20.png" alt="Last Page" /></a> </div> <a href="http://www.osti.gov/nle/topicpages">Index</a> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">321</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf16/poster_abs/P00176"> <span id="translatedtitle">Expansion of Facilities on the North Slope of Alaska in Time for the</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Expansion of Facilities on the North Slope of Alaska in Time for the Expansion of Facilities on the North Slope of Alaska in Time for the International Polar Year Zak, Bernard Sandia National Laboratories Ivey, Mark Sandia National Laboratories Zirzow, Jeffrey Sandia National Laboratories Brower, Walter UIC Science Division ARM/<span class="hlt">NSA</span> Ivanoff, James <span class="hlt">NSA</span> Whiteman, Doug <span class="hlt">NSA</span>/AAO Sassen, Kenneth University of Alaska Fairbanks Truffer-Moudra, Dana University of Alaska Fairbanks Category: Infrastructure & Outreach The International Polar Year (IPY; 2007-2008) will stimulate research in both polar regions, primarily focusing on the rapid climate-related changes occurring at high latitudes. In part in preparation for the IPY, facilities at the <span class="hlt">NSA</span> ACRF are undergoing expansion. In addition, with funding through NOAA, Phase 1 of the planned $60M Barrow Global Climate Change Research </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">322</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/meetings/2006/presentations"> <span id="translatedtitle">ARM - 2006 Science Team Meeting Presentations</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">from the ARM Archive Raymond McCord (PDF, 2MB) Joint Meeting of Instantaneous Radiative Flux (IRF) and Clouds with Low Optical Water Depths CLOWD Working Groups: <span class="hlt">NSA</span> Broadband...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">323</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/sites/nsa/docs/nsa_bsp.pdf"> <span id="translatedtitle">DRAFT Bear Safety Plan</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Bear Safety Plan June 2010 Bear Safety Plan June 2010 <span class="hlt">NSA</span>_bsp_Rev9.doc 1 Atmospheric Radiation Measurement Climate Research Facility/ North Slope of Alaska/Adjacent Arctic Ocean (ACRF/<span class="hlt">NSA</span>/AAO) Bear Safety Plan Background As a major part of DOE's participation in the US Global Change Research Program (USGCRP), the North Slope of Alaska (<span class="hlt">NSA</span>) and Adjacent Arctic Ocean (AAO) Climate Research Facility (ACRF) exists on the North Slope of Alaska with its Central Facility near the town of Barrow. A secondary facility exists at Atqasuk, a town 100km inland from Barrow. Other instrumentation locations in more remote areas on the North Slope may be established in later stages of the project. Polar bears, and to a lesser extent, brown bears (barren ground grizzly) are significant hazards within the ACRF/<span class="hlt">NSA</span>/AAO </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">324</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/4130277"> <span id="translatedtitle">PRESENTATIONS OF 1963 AEC-CONTRACTORS NUCLEAR MATERIALS MANAGEMENT MEETING, %HELD AT< IDAHO FALLS, IDAHO, OCTOBER 16-18, 1963</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">Fifteen papers presented at the Ninth Annual AEC and Contractor Nuclear Materials Management Meeting are given. Separate abstracts were prepared for eleven papers. Four papers were previously abstracted for <span class="hlt">NSA</span>. (M.C.G.)</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate">1963-10-10T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">325</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/4029430"> <span id="translatedtitle">Hazards control progress report No. 50, January--June 1975</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">Progress report for January through June 1975. Of the five progress reports and four technical notes, abstracts of nine items appear separately in ERA, and six appear in <span class="hlt">NSA</span>. (GHT)</p> <div class="credits"> <p class="dwt_author">Mendenhall, V.R. (ed.)</p> <p class="dwt_publisher"></p> <p class="publishDate">1975-08-15T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">326</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/home/comment/reply/9752"> <span id="translatedtitle">Reply to comment | OSTI, US Dept of Energy, Office of Scientific...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/home/">Office of Scientific and Technical Information (OSTI)</a></p> <p class="result-summary">Slide26 Submitted by gibsone on Thu, 2013-09-12 13:22 quicktabs-title FY2006-stip-jordan Slide26 NSAView Over 829,000 searchable <span class="hlt">NSA</span> records to be available NSAView is a...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">327</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/home/comment/reply/9315"> <span id="translatedtitle">Reply to comment | OSTI, US Dept of Energy, Office of Scientific...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/home/">Office of Scientific and Technical Information (OSTI)</a></p> <p class="result-summary">Reply to comment Slide17 Submitted by gibsone on Fri, 2013-08-30 07:29 FY2010-cendi-jordan Slide17 ecd Energy Citations Database: citations from 40s to present (<span class="hlt">NSA</span> and EDB...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">328</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf18/poster/P00066.pdf"> <span id="translatedtitle">PowerPoint Presentation</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Radiation Measurement (ARM) North Slope of Alaska (<span class="hlt">NSA</span>) site. This type of mixed-phase cloud is a water-dominated cloud layer with precipitating ice, yet they persist for...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">329</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/education/post/16857"> <span id="translatedtitle">ARM - Education Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Climate Change Kiosk Opening Ceremony Bookmark and Share People view the new ARM Climate Change Kiosk at the <span class="hlt">NSA</span> site. The ARM Education and Outreach team had a very successful...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">330</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/659"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary"><span class="hlt">NSA</span> Operations Manager. Mark has a B.S. in environmental engineering from New Mexico Tech and a M.S. and Ph.D. in electrical engineering from the University of New Mexico....</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">331</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/4726363"> <span id="translatedtitle">PLUTONIUM AS A POWER REACTOR FUEL. Proceedings of American Nuclear Society Topical Meeting, Richland, Washington, September 13 and 14, 1962</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">A total of twenty-eight papers was presented at the meeting. Nine of these papers were previously abstracted in <span class="hlt">NSA</span>. Separate abstracts were prepared for nineteen papers. (J.R.D.)</p> <div class="credits"> <p class="dwt_author">Dawson, F.G. comp.</p> <p class="dwt_publisher"></p> <p class="publishDate">1962-12-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">332</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/4818875"> <span id="translatedtitle">HEALTH PHYSICS DIVISION ANNUAL PROGRESS REPORT, FOR PERIOD ENDING JULY 31, 1961</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">Progress is reported in 26 papers on radioactive waste disposal, ecologicah research, radiation physics and dosimetry, internal dosimetry, and health physics technology. Twenty-five separate abstracts were prepared. One paper was previously abstracted for <span class="hlt">NSA</span>. (M.C.G.)</p> <div class="credits"> <p class="dwt_author">none,</p> <p class="dwt_publisher"></p> <p class="publishDate">1961-10-31T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">333</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/oha/downloads/fia-12-0034-matter-national-security-archive"> <span id="translatedtitle">FIA-12-0034 - In the Matter of National Security Archive | Department...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">documents relating to the Bonn Climate Change talks in August 2010. OIR conducted a search and located one responsive document. <span class="hlt">NSA</span> challenged the adequacy of the search and the...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">334</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/meetings/2008/presentations/0312/5_Walsh.pdf"> <span id="translatedtitle">PowerPoint Presentation</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">ARM-<span class="hlt">NSA</span> products to evaluate ARM-<span class="hlt">NSA</span> products to evaluate Arctic cloud and radiative simulations in global models John E.Walsh, Diane H. Portis, William L. Chapman Department of Atmospheric Sciences University of Illinois, Urbana, IL USA ARM Science Team Meeting, Norfolk, VA 12 March 2008 Objectives * Use ARM/<span class="hlt">NSA</span> measurements to assess simulated clouds and surface radiation fluxes in global models * Diagnose cloud/radiation performance based on characteristics of model parameterizations Motivation: Cloud-radiative forcing in atmospheric reanalyses * NCEP/NCAR * ERA40 (ECMWF) * NARR (North American Regional Reanalysis) * JRA-25 (Japan) Validation with ARM/<span class="hlt">NSA</span> data, 1999-2006 Cloud-Radiative-Forcing (CRF): Net surface radiation (SW + LW) with actual cloudiness minus clear-sky net surface radiation </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">335</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf16/extended_abs/long_cn1.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Analyses from <span class="hlt">TWP</span>-ICE Analyses from <span class="hlt">TWP</span>-ICE C.N. Long and J.H. Mather Pacific Northwest National Laboratory Richland, Washington N. Tapper and J. Beringer Monash University Melbourne, Australia B. Atkinson Australian Bureau of Meteorology Darwin, Australia Introduction Surface data collected during Tropical Warm Pool-International Cloud Experiment (<span class="hlt">TWP</span>-ICE) includes radiation and standard meteorological measurements at six remote sites, as well as those at the ARM Climate Research Facility (ACRF) Darwin site (Figure 1). Five of these remote sites include not only unshaded broadband hemispheric shortwave (SW) and longwave (LW) instruments, but also a multi- detector SW radiometer designed to simultaneously measure both the downwelling diffuse and total SW </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">336</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf19/poster/P00027.pdf"> <span id="translatedtitle">varble_arm09.pdf</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Max Reflectivity Samples Max Reflectivity Samples Max Reflectivity Samples Max Reflectivity Samples Altitude [km] Altitude [km] RH Regime ω Anom. Pressure [hPa] Pressure [hPa] Climatological Context for <span class="hlt">TWP</span>-ICE Convective Precipitation Features Adam Varble and Ed Zipser Department of Meteorology, University of Utah Objectives * Define kinematic and thermodynamic regimes that exist in Darwin during the wet season using k-means cluster analyses of ERA-Interim soundings * Compare convective properties of the regimes using 10 years of TRMM PR data * Put the <span class="hlt">TWP</span>-ICE IOP period into context using the Gunn Pt. CPOL radar and the constructed climatology * Attempt to explain differences in convective properties between <span class="hlt">TWP</span>-ICE and climatology Data and Methods * 1997/98-2006/07 DJFM ERA-Interim data </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">337</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf12/poster_abs/P00166"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Fair - Weather Cumuli Climatology at the <span class="hlt">TWP</span> ARM Site Fair - Weather Cumuli Climatology at the <span class="hlt">TWP</span> ARM Site Kollias, P. and Albrecht B.A., University of Miami Twelfth Atmospheric Radiation Measurement (ARM) Science Team Meeting Fair-weather cumuli are fundamental in regulating the vertical structure of water vapor and entropy in the lowest 2 km of the Earths atmosphere over vast areas of the oceans. Over two years of data from the mm-wavelength cloud radar, at the Nauru (<span class="hlt">TWP</span>-ARM) site, are analyzed and a statistical description of the field of fair weather cumulus is inferred. Frequency diagrams of cloud thickness, fractional coverage, updraft-downdraft magnitudes and cloud reflectivity are calculated for four different classes of fair weather cumuli. Seasonal patterns are identified and their relationship to the thermodynamic structure of the boundary layer (wet-dry </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">338</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf18/poster/P00019.pdf"> <span id="translatedtitle">Slide 1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Variability of Tropical Cirrus from 2006 <span class="hlt">TWP</span>-ICE Variability of Tropical Cirrus from 2006 <span class="hlt">TWP</span>-ICE Junshik Um, Greg M. McFarquhar, and Matt Freer University of Illinois, Urbana IL junum@earth.uiuc.edu 1. Introduction In-situ cloud data acquired during the 2006 Tropical Warm Pool - International Cloud Experiment (<span class="hlt">TWP</span>-ICE) are used to determine if the microphysical properties of tropical cirrus formed under differing conditions can be characterized in terms of prognostic variables in large-scale models such as temperature and ice water content (IWC) To accomplish this, the spatial variability (horizontal and vertical) of microphysical properties (IWC, habit distribution, size distribution, median mass diameter D mm ) is examined and contrasted for different types of cirrus (convective vs. non- convective; aged vs. fresh), </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">339</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf18/poster/P00049.pdf"> <span id="translatedtitle">Microsoft PowerPoint - ARM_2008_poster_Wu_DelGenio</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">and GISS SCM Simulations of Convective Updrafts During <span class="hlt">TWP</span>-ICE and GISS SCM Simulations of Convective Updrafts During <span class="hlt">TWP</span>-ICE Jingbo Wu (Columbia U.), Anthony D. Del Genio (NASA/GISS) SUMMARY: Diagnosis of convective updraft speeds in global climate models is important for two reasons. First, the strength of cumulus updrafts determines the vertical convective condensate transport and the detrainment into anvils whose microphysical and radiative properties are important to climate feedbacks. Second, cumulus updraft speeds are also diagnostic of various severe weather phenomena, such as lightning, that contribute to ozone and carbonaceous aerosol climate forcing. The <span class="hlt">TWP</span>-ICE IOP, with distinctive convection types of weak vs. strong and deep vs. shallow convection, provides a good opportunity to evaluate a model's ability to simulate variable convective </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">340</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00094.pdf"> <span id="translatedtitle">arm2007_poster_wu_final.ppt</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">POSTER TEMPLATE BY: POSTER TEMPLATE BY: www.PosterPresentations.com Convection regimes during <span class="hlt">TWP</span>-ICE and in the GISS SCM Jingbo Wu (Columbia U.), Anthony D. Del Genio (NASA/GISS), and Audrey B. Wolf (Columbia U.) 1. Introduction The <span class="hlt">TWP</span>-ICE IOP included an early "active monsoon" period with an apparent maritime style of convection, and a late "break" period with occasional intense continental convection. This IOP thus offers the opportunity to understand physical processes that cause differences in convective intensity and the ability of GCM cumulus parameterizations to simulate these differences, which are hypothesized to influence detrainment into radiatively important anvil clouds. 2. Observations Figure 1: Overview of the <span class="hlt">TWP</span>-ICE array (J. 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href="http://www.osti.gov/nle/topicpages">Index</a> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">341</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/meetings/2009/presentations/0401/6_COLLIS.pdf"> <span id="translatedtitle">Presentation Title, Arial Regular 29pt Sub title, Arial Regular 24pt</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Centre for Australian Weather and Climate Research Centre for Australian Weather and Climate Research A partnership between CSIRO and the Bureau of Meteorology Updraft Characteristics of Convection During <span class="hlt">TWP</span>-ICE and Links to Microphysical Habits Scott Collis, Alain Protat, Peter May and Kao-Shen Chung 19 th ARM Science Team Meeting www.cawcr.gov.au Introduction/Program goals Link between updraft characteristics and anvil Cloud properties Link between updraft characteristics and anvil Cloud properties Introduction/Program goals <span class="hlt">TWP</span>-ICE Forcing data Models Updrafts Link between updraft characteristics and anvil Cloud properties Introduction/Program goals <span class="hlt">TWP</span>-ICE Forcing data Models Updrafts Doppler radar velocity retrievals Polarimetric radar Microphysics retrievals The Centre for Australian Weather and Climate Research </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">342</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf09/extended_abs/feltz_wf.pdf"> <span id="translatedtitle">feltz-99.PDF</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">+ GOES Retrievals at the <span class="hlt">SGP</span> ARM Site: SCM Data + GOES Retrievals at the <span class="hlt">SGP</span> ARM Site: SCM Data Assimilation and Convective Forecasting Utility W. F. Feltz, R. O. Knuteson, H. E. Revercomb, and H. B. Howell University of Wisconsin-Madison Cooperative Institute for Meteorological Satellite Studies Madison, Wisconsin Introduction Four additional Atmospheric Emitted Radiance Interferometer (AERI) systems have been deployed at the U.S. Department of Energy's (DOE's) Atmospheric Radiation Measurement (ARM) Southern Great Plains Cloud And Radiation Testbed (<span class="hlt">SGP</span> CART) site boundary facilities. The AERI + GOES (Geostationary Operational Environmental Satellite) temperature and water vapor retrieval product is now operational at Pacific Northwest National Laboratory (PNNL) allowing continuous monitoring of </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">343</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/sites/twp/instruments"> <span id="translatedtitle">ARM - Site Instruments</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">PacificInstruments PacificInstruments <span class="hlt">TWP</span> Related Links Facilities and Instruments Manus Island Nauru Island Darwin, AUS ES&H Guidance Statement Operations Science Field Campaigns Year of Tropical Convection Visiting the Site <span class="hlt">TWP</span> Fact Sheet Images Information for Guest Scientists Contacts Instruments : Tropical Western Pacific [ Installed at 3 facilities ] AERI Atmospheric Emitted Radiance Interferometer Radiometric Browse Plots Browse Data [ Installed at 2 facilities ] CSAPR C-Band ARM Precipitation Radar Cloud Properties Browse Data [ Installed at 3 facilities ] CSPHOT Cimel Sunphotometer Aerosols, Radiometric Browse Data [ Single installation ] DISDROMETER Impact Disdrometer Surface Meteorology Browse Plots Browse Data [ Single installation ] DL Doppler Lidar Cloud Properties Browse Data [ Installed at 3 facilities ] </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">344</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/sites/twp/C3/instruments"> <span id="translatedtitle">ARM - Site Instruments</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Darwin SiteInstruments Darwin SiteInstruments <span class="hlt">TWP</span> Related Links Facilities and Instruments Manus Island Nauru Island Darwin, AUS ES&H Guidance Statement Operations Science Field Campaigns Year of Tropical Convection Visiting the Site <span class="hlt">TWP</span> Fact Sheet Images Information for Guest Scientists Contacts Instruments : Central Facility, Darwin, Australia [ Single installation ] AERI Atmospheric Emitted Radiance Interferometer Radiometric Browse Plots Browse Data [ Single installation ] CSPHOT Cimel Sunphotometer Aerosols, Radiometric Browse Data [ Single installation ] DISDROMETER Impact Disdrometer Surface Meteorology Browse Plots Browse Data [ Single installation ] DL Doppler Lidar Cloud Properties Browse Data [ Single installation ] GNDRAD Ground Radiometers on Stand for Upwelling Radiation Radiometric Browse Plots </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">345</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf12/extended_abs/long-cn.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Variability Across the ARM <span class="hlt">SGP</span> Area Variability Across the ARM <span class="hlt">SGP</span> Area by Temporal and Spatial Scale C. N. Long and T. P. Ackerman Pacific Northwest National Laboratory J. E. Christy Columbia University New York, New York Introduction The Surface Cloud Grid (SfcCldGrid) value-added product (VAP) uses the output of the Shortwave Flux Analysis VAP (Long and Ackerman 2000, Long et al. 1999, Long 2001) at 15-minute resolution for each of the 21 surface radiometer sites of the Atmospheric Radiation Measurement (ARM) Southern Great Plains (<span class="hlt">SGP</span>) network area as input. The SfcCldGrid VAP uses the Analytic Approximation interpolation technique of Caracena (1987) to produce a 0.25° × 0.25° grid across the ARM <span class="hlt">SGP</span> area at 15-minute resolution. (More information about the SfcCldGrid VAP, and an analysis of the interpola- </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">346</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf07/extended_abs/peppler_ra.pdf"> <span id="translatedtitle">Section 90</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary"><span class="hlt">SGP</span> Site Scientist Team Data Quality <span class="hlt">SGP</span> Site Scientist Team Data Quality Assessment Activities R. A. Peppler and M. E. Splitt Cooperative Institute for Mesoscale Meteorological Studies University of Oklahoma Norman, Oklahoma Introduction Data Quality Assessment Tools A primary task of the Site Scientist Team (SST) of the Following is a discussion of data quality performance metrics, Southern Great Plains (<span class="hlt">SGP</span>) CART site is to analyze and data quality graphical displays, and calibration and main- assess the quality of the various <span class="hlt">SGP</span> data streams. This task tenance information summaries. is performed in conjunction with other groups within ARM such as Instrument Mentors (responsible for individual instru- ments), various Data and Science Integration Team (DSIT) members (responsible for multiple data stream comparisons </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">347</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf12/poster_abs/P00191"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">The Clear-Sky Diffuse 'Problem' at <span class="hlt">SGP</span>: RSS Data & Analysis The Clear-Sky Diffuse 'Problem' at <span class="hlt">SGP</span>: RSS Data & Analysis Harrison, L., Kiedron, P., and Min, Q., State University of new York, Albany Twelfth Atmospheric Radiation Measurement (ARM) Science Team Meeting We analyze the spectral RSS data from the fall of 1999, when there were an unusual series of clear-sky cloud-free days at <span class="hlt">SGP</span>. The RSS makes measurements of the spectral diffuse/direct ratio which are independent of calibration. We also extract typical optical depth analyis data from Langley regressions, and we retrieve column NO2 from correlation spectroscopy. We show that column NO2 is often well above clean-climatological background at <span class="hlt">SGP</span>, and that this interacts with simple forms of aerosol-optical depth retrievals (which do not account for this) </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">348</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/campaigns/sgp2011midlatcloud"> <span id="translatedtitle">ARM - Field Campaign - Midlatitude Continental Convective Clouds Experiment</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Experiment (MC3E) Experiment (MC3E) Campaign Links Science Plan MC3E Website Related Campaigns Midlatitude Continental Convective Clouds Experiment: 2DVD Support 2011.04.22, Schwaller, <span class="hlt">SGP</span> Midlatitude Continental Convective Clouds Experiment (MC3E): Airborne Instruments 2011.04.22, Poellot, AAF Midlatitude Continental Convective Clouds Experiment (MC3E): Multi-Frequency Profilers 2011.04.22, Williams, <span class="hlt">SGP</span> Midlatitude Continental Convective Clouds Experiment: Parsivel Disdrometer Support 2011.04.22, Schwaller, <span class="hlt">SGP</span> Midlatitude Continental Convective Clouds Experiment (MC3E): Inner Domain Thermodynamic Profiling during MC3E 2011.04.22, Turner, <span class="hlt">SGP</span> Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Campaign : Midlatitude Continental Convective Clouds Experiment (MC3E) </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">349</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf15/poster_abs/P00156"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents: Comparison of ECMWF</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Comparison of ECMWF Model and ARSCL Cloudiness at the ARM <span class="hlt">SGP</span> site Comparison of ECMWF Model and ARSCL Cloudiness at the ARM <span class="hlt">SGP</span> site Kollias, Pavlos RSMAS/University of Miami Albrecht, Bruce University of Miami The Department of Energy (DOE) Atmospheric Radiation Measurements (ARM) Program operates a comprehensive suite of active remote sensors at Southern Great Plains (<span class="hlt">SGP</span>) in Oklahoma since 1996 to detect all hydrometeors in the atmospheric column above. Due to its location, the ARM <span class="hlt">SGP</span> site cloud and precipitation climatology it is believed to be representative of mid-latitudes. Long-term (6.5 years) observations from this ARM site are used to provide a cloud and precipitation climatology. A cloud classification scheme based on cloud base height, fractional coverage, cloud thickness, cloud reflectivity and precipitation detection at the </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">350</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/poster_abs/P00168"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">GPS Measured Water Vapor Variability at the ARM <span class="hlt">SGP</span> CF GPS Measured Water Vapor Variability at the ARM <span class="hlt">SGP</span> CF Braun, J. (a), Rocken, C. (a), and Schmid, B. (b), UCAR (a), BAER (b) Eleventh Atmospheric Radiation Measurement (ARM) Science Team Meeting Ground based Global Positioning System (GPS) stations can measure precipitable water vapor (PWV) and slant water vapor (SWV). SWV is the integrated amount of water vapor along the slant path from the GPS transmitter to the station. The ARM program has sponsored the University Corporation for Atmospheric Research (UCAR) to install and operate a network of single frequency GPS receivers at the Southern Great Plains (<span class="hlt">SGP</span>) Central Facility (CF). Fourteen stations were installed in 1999, and an additional nine stations in 2000. The entire network covers approximately 40 square kilometers roughly centered around the <span class="hlt">SGP</span> CF. This </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">351</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf16/extended_abs/orr_bw.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Figure 2. The infrared sky imager at the <span class="hlt">SGP</span> CF. Dynamic Rain Gauge Calibrator A new dynamic rain gauge calibrator has been built and is being used to calibrate rain...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">352</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/2963"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">News Severe Storms the Focus of VORTEX Operations staff at the <span class="hlt">SGP</span> site release weather balloons 4 times a day, Monday through Friday, all year round. During VORTEX2, they...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">353</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf13/poster_abs/P00151"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">MOD06 Cloud Products and the ARM <span class="hlt">SGP</span> Zhang, Y.(a) and Mace, G.G.(b), University of Utah (a), University of Utah (b) Thirteenth Atmospheric Radiation Measurement (ARM) Science...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">354</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/828"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">May 31, 2006 [Facility News] May 31, 2006 [Facility News] New Shortwave Spectroradiometer Deployed at <span class="hlt">SGP</span> Bookmark and Share A ceiling port in the <span class="hlt">SGP</span> Optical Trailer houses the optic element of the SWS, which connects to the spectrometer inside the trailer via fiber optic cable. A ceiling port in the <span class="hlt">SGP</span> Optical Trailer houses the optic element of the SWS, which connects to the spectrometer inside the trailer via fiber optic cable. In late April, a new Shortwave Spectroradiometer (SWS) began operating at the ARM Southern Great Plains (<span class="hlt">SGP</span>) site. The instrument measures the zenith solar spectral radiance (1.4° field of view) between 300-2200 nm. The SWS incorporates two Zeiss miniature monolithic spectrometers having a spectral resolution of 8 nm in the range 300-975 nm, and 12 nm in the range </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">355</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf12/poster_abs/P00043"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Evaluation of Terra Aerosol and Water Vapor Measurements Using ARM <span class="hlt">SGP</span> Data Evaluation of Terra Aerosol and Water Vapor Measurements Using ARM <span class="hlt">SGP</span> Data Ferrare, R.A.(a), Brasseur, L.H.(b), Clayton, M.B.(b), Turner, D.D.(c), Remer, L.(d), and Gao, B.C.(e), NASA Langley (a), SAIC (b), Pacific Northwest National Laboratory (c), NASA Goddard (d), Naval Research Laboratory (e) Twelfth Atmospheric Radiation Measurement (ARM) Science Team Meeting Measurements from the Department of Energy Atmospheric Radiation Measurement (ARM) Southern Great Plains (<span class="hlt">SGP</span>) site are used to evaluate atmospheric measurements derived from NASA's Moderate-Resolution Imaging Spectroradiometer (MODIS) and Multiangle Imaging Spectroradiometer (MISR) sensors on board the Terra satellite. MODIS and MISR AOT retrievals are evaluated using ARM <span class="hlt">SGP</span> Cimel Sun photometer and MultiFilter Rotating </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">356</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/poster_abs/P00040"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Comparison of MM5 Forecast Shortwave Radiation with ARM <span class="hlt">SGP</span> Data Comparison of MM5 Forecast Shortwave Radiation with ARM <span class="hlt">SGP</span> Data Armstrong, M.A. and Ellingson, R.G., University of Maryland Eleventh Atmospheric Radiation Measurement (ARM) Science Team Meeting The performance of the Pennsylvania State University-National Center for Atmospheric Research Mesoscale Model 5 (MM5), in particular the shortwave downwelling (SW) flux calculations, is examined in this paper. Selected quantities output from the MM5 were compared with ARM <span class="hlt">SGP</span> data gathered during the SCM intensive observation period (IOP) from June 18 to July 18, 1997. MM5 was run 29 times with a forecast length of 24 hours. The data were saved and then compared to radiosonde and pyranometer data. SW flux calculated from the MM5 deviated severely from that observed at the <span class="hlt">SGP</span> </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">357</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/1008"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">15, 2005 [Facility News] 15, 2005 [Facility News] Aging, Overworked Computer Network at <span class="hlt">SGP</span> Gets Overhauled Bookmark and Share This aerial map of instruments deployed at the <span class="hlt">SGP</span> Central Facility provides an indication of the computer resources needed to manage data at the site, let alone communicate with other ARM sites. This aerial map of instruments deployed at the <span class="hlt">SGP</span> Central Facility provides an indication of the computer resources needed to manage data at the site, let alone communicate with other ARM sites. Established as the first ARM research facility in 1992, the Southern Great Plains (<span class="hlt">SGP</span>) site in Oklahoma is the "old man on the block" when it comes to infrastructure. Though significant improvements have been made to facilities and equipment throughout the years, the computer network at the </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">358</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/abs/10.1175/1520-0426%282000%29017%3C0312%3AEOASMO%3E2.0.CO%3B2?prevSearch=%5BFulltext%3A+national+AND+energy+AND+technology+AND+lab%5D&searchHistoryKey="> <span id="translatedtitle">Enhancement of ARM Surface Meteorological Observations during the Fall 1996 Water Vapor Intensive Observation Period</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">This work describes in situ moisture sensor comparisons that were performed in conjunction with the first Water Vapor Intensive Observation Period (IOP) conducted at the Atmospheric Radiation Measurement (ARM) Program Southern Great Plains (<span class="hlt">SGP</span>) ...</p> <div class="credits"> <p class="dwt_author">Scott J. Richardson; Michael E. Splitt; Barry M. Lesht</p> <p class="dwt_publisher"></p> <p class="publishDate">2000-03-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">359</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://pangea.stanford.edu/ERE/pdf/IGAstandard/SGW/2011/zaher.pdf"> <span id="translatedtitle">PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 31 -February 2, 2011</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 31 - February 2, 2011 <span class="hlt">SGP</span>-TR-191 ASSESSMENT OF LOW-TEMPERATURE GEOTHERMAL Fujimitsu and Sachio Ehara Geothermic Laboratory, Earth Resources Engineering Department, Kyushu University</p> <div class="credits"> <p class="dwt_author">Stanford University</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">360</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf10/extended_abs/lesins_g.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Five Years of Clear-Sky Solar Radiation Measurements and Aerosol Forcing at the <span class="hlt">SGP</span> ARM Site G. Lesins and Q. Fu Department of Oceanography Dalhousie University Halifax, Nova...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_17");' href="#" title="Previous Page"> <img id="PreviousPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.previous.18x20.png" alt="Previous Page" /></a> <span id="PageLinks" class="pageLinks"> <span> <a onClick='return showDiv("page_1");' href="#">1</a> <a onClick='return showDiv("page_2");' href="#">2</a> 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</div> <a href="http://www.osti.gov/nle/topicpages">Index</a> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">361</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/campaigns/sgp1999sumscm"> <span id="translatedtitle">ARM - Field Campaign - Summer Single Column Model IOP</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">July 12-22, 1999, in conjunction with the <span class="hlt">SGP</span>99 Campaign by the U.S. Department of Agriculture. The purpose of this 10-day SCM effort was to test how well remote sensing...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">362</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/abs/10.1175/1520-0469%282002%29059%3C1135%3AVOAOPA%3E2.0.CO%3B2?prevSearch=%5BFulltext%3A+flag+AND+tubes%5D&searchHistoryKey="> <span id="translatedtitle">Variability of Aerosol Optical Properties at Four North American Surface Monitoring Sites</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">Aerosol optical properties measured over several years at surface monitoring stations located at Bondville, Illinois (BND); Lamont, Oklahoma (<span class="hlt">SGP</span>); Sable Island, Nova Scotia (WSA); and Barrow, Alaska (BRW), have been analyzed to determine the ...</p> <div class="credits"> <p class="dwt_author">David J. Delene; John A. Ogren</p> <p class="dwt_publisher"></p> <p class="publishDate">2002-03-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">363</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/640"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Exchange Researchers installed a continuous 222Rn monitor at the base of the 60-meter tower at the <span class="hlt">SGP</span> Central Facility. A sampling tube connected to the tower supplies air to...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">364</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf14/poster_abs/P00191"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Comparison of In-Situ, Airborne and Surface Remote Sensing of Cloud Droplet Size and Liquid Water Path Over <span class="hlt">SGP</span> CART During the Aerosol IOP Pilewskie, P.(a), Feingold, G.(b),...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">365</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/2008JAMC1949.1"> <span id="translatedtitle">Cirrus Microphysical Properties and Air Motion Statistics Using Cloud Radar Doppler Moments. Part II: Climatology</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">The algorithm described in Part I has been applied to the millimeter cloud radar observations from January 1999 to December 2005 at the Atmospheric Radiation Measurement Program (ARM) Southern Great Plains (<span class="hlt">SGP</span>) and Tropical Western Pacific (...</p> <div class="credits"> <p class="dwt_author">Min Deng; Gerald G. Mace</p> <p class="dwt_publisher"></p> <p class="publishDate">2008-12-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">366</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/instruments/mfr"> <span id="translatedtitle">ARM - Instrument - mfr</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary"><span class="hlt">SGP</span> C1 Browse Data Central Facility, Lamont, OK ARM Mobile Facility PVC M1 Browse Data Highland Center, Cape Cod MA; AMF 1 Contact(s) Gary Hodges (303) 497-6460 Gary.Hodges@noaa...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">367</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/data/datastreams/dlusr"> <span id="translatedtitle">ARM - Datastreams - dlusr</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">timeoffset ( time ) Locations Southern Great Plains <span class="hlt">SGP</span> C1 Browse Data Central Facility, Lamont, OK ARM Mobile Facility PVC M1 Browse Data Highland Center, Cape Cod MA; AMF 1...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">368</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf09/extended_abs/peppler_ra.pdf"> <span id="translatedtitle">peppler-99.PDF</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Ninth ARM Science Team Meeting Proceedings, San Antonio, Texas, March 22-26, 1999 1 Identification and Analysis of the 1998 Central American Smoke Event at the ARM <span class="hlt">SGP</span> CART Site R....</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">369</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://escholarship.org/uc/item/0j9561zd?query=washington+AND+dc"> <span id="translatedtitle">US military expenditures to protect the use of Persian Gulf oil for motor vehicles</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">Defense Information, Washington, DC August 1 /www. cdi.org/Research Service, Washington, DC, June 16. /www.fas.org/<span class="hlt">sgp</span>/for the Future, Washington, DC. Boyd, R. , Chermak, J.M. ,</p> <div class="credits"> <p class="dwt_author">Delucchi, Mark; Murphy, James</p> <p class="dwt_publisher"></p> <p class="publishDate">2008-01-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">370</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/fact-sheets/docs/doe-sc-arm-11-016.pdf"> <span id="translatedtitle">FACT SHEET U.S. Department of Energy</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">largest and most extensive climate research field site. Deployment of the first instrumentation to the <span class="hlt">SGP</span> site occurred in the spring of 1992, and the site was dedicated in...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">371</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf14/poster_abs/P00181"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">The entire year 2000 at <span class="hlt">SGP</span> is planned to be processed by the time of the time of the Science Team Meeting, and results from these runs will be presented. This version should...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">372</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/abs/10.1175/1520-0450%282003%29042%3C0584%3ANPOTMA%3E2.0.CO%3B2?prevSearch=%5BFulltext%3A+home+AND+usage%5D&searchHistoryKey="> <span id="translatedtitle">Near-Continuous Profiling of Temperature, Moisture, and Atmospheric Stability Using the Atmospheric Emitted Radiance Interferometer (AERI)</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">The Department of Energy Atmospheric Radiation Measurement Program (ARM) has funded the development and installation of five ground-based atmospheric emitted radiance interferometer (AERI) systems at the Southern Great Plains (<span class="hlt">SGP</span>) site. The ...</p> <div class="credits"> <p class="dwt_author">W. F. Feltz; W. L. Smith; H. B. Howell; R. O. Knuteson; H. Woolf; H. E. Revercomb</p> <p class="dwt_publisher"></p> <p class="publishDate">2003-05-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">373</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf16/extended_abs/alexandrov_m.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">CIMEL sun-photometer co-located with the MFRSR at the <span class="hlt">SGP</span> Central Facility. Precipitable water vapor column amounts are determined from the direct normal irradiances in the 940 nm...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">374</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/JCLI-D-12-00223.1"> <span id="translatedtitle">Multiyear Summertime Observations of Daytime Fair-Weather Cumuli at the ARM Southern Great Plains Facility</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">A long data record (14 yr) of ground-based observations at the Atmospheric Radiation Measurement Program (ARM) Southern Great Plains (<span class="hlt">SGP</span>) site is analyzed to document the macroscopic and dynamical properties of daytime fair-weather cumulus clouds ...</p> <div class="credits"> <p class="dwt_author">Arunchandra S. Chandra; Pavlos Kollias; Bruce A. Albrecht</p> <p class="dwt_publisher"></p> <p class="publishDate">2013-12-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">375</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/programdocs/doe-sc-arm-p-06-017.pdf"> <span id="translatedtitle">Microsoft Word - fourthqmetric 2.doc</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">(middle),AM2(bottom) 5 2. Comparison of cloud fraction at the <span class="hlt">SGP</span>. (CAM3Blue, AM2Black). Correlation (top), RMS (middle), Bias (bottom) 6 3. Comparison of cloud fraction at...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">376</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf15/poster_abs/P00141"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents: Scanning...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">November 2002 rejoined the program to participate in the <span class="hlt">SGP</span> leg of the ARM-UAV "Grand Tour". S-HIS spectral coverage is 580-3000 cm-1 with a resolution of 0.5 cm-1, and spatially...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">377</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/JCLI-D-11-00380.1"> <span id="translatedtitle">AtmosphereLand Surface Interactions over the Southern Great Plains: Characterization from Pentad Analysis of DOE ARM Field Observations and NARR</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">The Department of Energy Atmospheric Radiation Measurement Program (ARM) Southern Great Plains (<span class="hlt">SGP</span>) site data are analyzed to provide insight into atmosphereland surface interactions generating summertime precipitation variability. Pentad-...</p> <div class="credits"> <p class="dwt_author">Alfredo Ruiz-Barradas; Sumant Nigam</p> <p class="dwt_publisher"></p> <p class="publishDate">2013-02-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">378</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/abs/10.1175/JCLI-D-12-00223.1?prevSearch=%5BFulltext%3A+brookhaven+AND+annual+AND+report%5D&searchHistoryKey="> <span id="translatedtitle">Multi-year, Summertime Observations of Daytime Fair-Weather Cumuli at the ARM Southern Great Plains facility</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">A long data record (14-year) of ground-based observations at the Atmospheric Radiation Measurement (ARM) program Southern Great Plains (<span class="hlt">SGP</span>) site is analyzed to document the macroscopic and dynamical properties of daytime fair-weather cumulus ...</p> <div class="credits"> <p class="dwt_author">Arunchandra S. Chandra; P. Kollias; B. A. Albrecht</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">379</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/sites/sgp"> <span id="translatedtitle">Southern Great Plains</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">govSitesSouthern Great Plains govSitesSouthern Great Plains <span class="hlt">SGP</span> Related Links Facilities and Instruments Central Facility Boundary Facility Extended Facility Intermediate Facility Radiometric Calibration Facility Geographic Information ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Fact Sheet Images Information for Guest Scientists Contacts Southern Great Plains <span class="hlt">SGP</span> Central Facility, Lamont, OK 36° 36' 18.0" N, 97° 29' 6.0" W Altitude: 320 meters The Southern Great Plains (<span class="hlt">SGP</span>) site was the first field measurement site established by DOE's Atmospheric Radiation Measurement (ARM) Program. Scientists are using the information obtained from the <span class="hlt">SGP</span> to improve cloud and radiative models and parameterizations and, thereby, the performance of atmospheric general circulation models used for climate research. </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">380</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf05/extended_abs/mace3_gg.pdf"> <span id="translatedtitle">X:\\ARM_19~1\\P185-192.WPD</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Micropulse lidar cloud base frequency. A One-Year Cloud Climatology Using Data from the Southern Great Plains (<span class="hlt">SGP</span>) Site Micropulse Lidar G. G. Mace and T. P. Ackerman Penn State...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_18");' href="#" title="Previous Page"> <img id="PreviousPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.previous.18x20.png" alt="Previous Page" /></a> <span id="PageLinks" class="pageLinks"> <span> <a onClick='return showDiv("page_1");' href="#">1</a> <a onClick='return showDiv("page_2");' href="#">2</a> <a onClick='return showDiv("page_3");' 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href="http://www.osti.gov/nle/topicpages">Index</a> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">381</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf19/poster/P00051.pdf"> <span id="translatedtitle">Microsoft PowerPoint - ferrare_STM_2009_poster [Compatibility...</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">clouds? H th i ti l t d t h i Approach * Use combination of advanced ground (<span class="hlt">SGP</span> Raman Lidar) and airborne (NASALaRC HSRL) lidars and * Lidar measurements show increases in...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">382</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf05/extended_abs/mace_gg.pdf"> <span id="translatedtitle">X:\\ARM_19~1\\P155-184.WPD</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">of the primary reasons that the Southern Great Plains (<span class="hlt">SGP</span>) site is located in Lamont, Oklahoma, is because Lamont is at the approximate center of the NOM Wind Profiler...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">383</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf05/extended_abs/zhong_s.pdf"> <span id="translatedtitle">X:\\ARM_19~1\\P377-392.WPD</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">wind profiler demonstration network. The <span class="hlt">SGP</span> CART central facility is located at Lamont, Oklahoma. A Case Study of the Great Plains Low-Level Jet Using Wind Profiler Network Data...</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">384</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/sites/nsa/docs/nsa_dup.pdf"> <span id="translatedtitle"> </span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">1 1 Duplex Rules June 2010 Atmospheric Radiation Measurement Climate Research Facility/ North Slope of Alaska/Adjacent Arctic Ocean (ACRF/<span class="hlt">NSA</span>/AAO) Duplex Rules Who can stay in the duplex? The rental for the duplex is paid out of the ACRF/<span class="hlt">NSA</span>/AAO Site Manager's (SM's) Site Development and Operations budget at Sandia National Laboratories. ACRF personnel working directly on tasks for the ACRF/<span class="hlt">NSA</span>/AAO Site will have priority in the use of the duplex. Other ACRF users will be accommodated on an as-available basis. A total of six bedrooms are now available in the duplex; 4 rooms have twin bunk beds, 1 room has 2 twin beds, and 1 room has a queen size bed. The duplex can accommodate 11 people with doubling up in the rooms that have bunk and twin beds. The Site Manager, Mark Ivey, will confirm extension of duplex </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">385</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/sites/nsa"> <span id="translatedtitle">North Slope of Alaska</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">govSitesNorth Slope of Alaska govSitesNorth Slope of Alaska <span class="hlt">NSA</span> Related Links Facilities and Instruments Barrow Atqasuk ES&H Guidance Statement Operations Science Field Campaigns Visiting the Site Images Information for Guest Scientists Contacts North Slope of Alaska Barrow: 71° 19' 23.73" N, 156° 36' 56.70" W Atqasuk: 70° 28' 19.11" N, 157° 24' 28.99" W The North Slope of Alaska (<span class="hlt">NSA</span>) site is providing data about cloud and radiative processes at high latitudes. Centered at Barrow and extending to the south (to the vicinity of Atqasuk), west (to the vicinity of Wainwright), and east (towards Oliktok), the <span class="hlt">NSA</span> site has become a focal point for atmospheric and ecological research activity on the North Slope. The principal instrumented facility was installed near Barrow in 1997, </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">386</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf14/poster_abs/P00139"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Winter Surface Radiative Energy Exchange at <span class="hlt">NSA</span>: Cloudy vs. Clear Sky Winter Surface Radiative Energy Exchange at <span class="hlt">NSA</span>: Cloudy vs. Clear Sky Stramler, K.(a), Del Genio, A.D.(b), and Rossow, W.(b), Columbia University (a), NASA/GISS (b) Thirteenth Atmospheric Radiation Measurement (ARM) Science Team Meeting ARM measurements at Point Barrow, Alaska show that atmospheric emission drives the winter variability of the surface radiative energy exchange, as the incursion of air masses of differing properties alternately warm and cool the snow surface and the snow-ground interface. The magnitude of the surface radiative energy exchange, however, appears to be in part dictated by the more slowly varying sub-surface temperatures. This is most evident when observing the inter-annual variability of clear-sky surface net longwave radiation at <span class="hlt">NSA</span>; winter cloudy-sky surface net longwave radiation </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">387</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf09/poster_abs/P00086"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Cloud and Radiative Properties Derived Over the ARM <span class="hlt">NSA</span> Domain From AVHRR Cloud and Radiative Properties Derived Over the ARM <span class="hlt">NSA</span> Domain From AVHRR Data Heck, P.W., Nguyen, L., Smith, W. L., Jr., Ayers, J.K., Doelling, D.R., and Spangenberg, D.A., Analytical Services and Materials, Inc.; Minnis, P., and Young, D.F., National Aeronautics and Space Administration-Langley Research Center Ninth Atmospheric Radiation Measurement (ARM) Science Team Meeting The Atmospheric Radiation Measurement (ARM) Program's polar sites on the North Slope of Alaska (<span class="hlt">NSA</span>) measure time series of various atmospheric, cloud and radiative properties over a few selected areas. Satellite data are needed to provide measurements of similar properties between the sites and to estimate the radiation budget at the top of the atmosphere. Over the other ARM sites in the central United States and the Pacific, geostationary </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">388</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00030.pdf"> <span id="translatedtitle">NCEP:</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">surface net radiation: surface net radiation: cloudy sky - clear sky cloud fraction (%) cloud fraction (%) cloud fraction (%) cloud fraction (%) cloud fraction (%) ARM/<span class="hlt">NSA</span> vs. reanalysis summmaries NCEP: shortwave flux NCEP: longwave flux ARM/<span class="hlt">NSA</span> validation of Arctic clouds and radiative impacts in reanalyses John E. Walsh, William L. Chapman and Diane H. Portis University of Illinois at Urbana-Champaign http://igloo.atmos.uiuc.edu/ARM/ Objectives: -- use ARM/<span class="hlt">NSA</span> measurements to assess reanalysis-derived surface radiation fluxes and clouds at the Barrow site -- evaluate cloud/radiative forcing in the reanalyses -- compare cloud/radiative parameterizations in each model Reanalysis years Center NCEP 1948-2006 National Center for Env. Prediction / National Center for Atmos. Research (USA) </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">389</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/highlights/RMTM1/view"> <span id="translatedtitle">Research Highlight</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Comparisons Between Radiosondes and Remote Sensors During the 2004 <span class="hlt">NSA</span> Comparisons Between Radiosondes and Remote Sensors During the 2004 <span class="hlt">NSA</span> Arctic Winter Radiometric Experiment Submitter: Westwater, E. R., University of Colorado Area of Research: Atmospheric Thermodynamics and Vertical Structures Working Group(s): Radiative Processes Journal Reference: Mattioli, V, ER Westwater, D Cimini, JS Liljegren, BM Lesht, SI Gutman, and FJ Schmidlin. 2007. "Analysis of radiosonde and ground-based remotely sensed PWV data from the 2004 North Slope of Alaska Arctic Winter Radiometric Experiment." Journal of Atmospheric and Oceanic Technology 243: 415-431. Description of radiosondes launched during the 2004 <span class="hlt">NSA</span> Arctic Winter Radiometric Experiment. Dual-radiosonde launch of the Vaisala RS90 and Chilled Mirror radiosondes is pictured here. </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">390</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf15/poster_abs/P00136"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents: Deployment of a</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Deployment of a scintillometer for optical turbulence investigation at <span class="hlt">NSA</span> Deployment of a scintillometer for optical turbulence investigation at <span class="hlt">NSA</span> - Barrow Moudry, Dana University of Alaska Fairbanks Sassen, Kenneth University of Alaska Fairbanks Vaucher, Gail Army Research Laboratory Zak, Bernard Sandia National Laboratories The University of Alaska Fairbanks in collaboration with the White Sands Army Research Lab deployed a reciprocal-path scintillometer to the ARM - <span class="hlt">NSA</span> site at Barrow in fall 2004 for investigation of optical turbulence over the course of a year. The instrument consists of a transmitter and a receiver located approximately 1km apart. The instrument transmitter includes two arrays of nearIR LEDs which emit light in a 125-Hz pulsed mode. The receiver measures the temporal variability of the radiation after </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">391</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/sites/prod/files/oha/FOIA/FIA-12-0034.pdf"> <span id="translatedtitle">Microsoft Word - FIA-12-0034.docx</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">National Security Archive ) National Security Archive ) ) Filing Date: June 12, 2012 ) Case No.: FIA-12-0034 ) ________________________ ___________ ) Issued: July 9, 2012 ______________ Decision and Order _______________ This Decision concerns an Appeal that the National Security Archive (<span class="hlt">NSA</span>) filed in response to a determination that the Department of Energy's (DOE) Office of Information Resources (OIR) issued to it. In that determination, the OIR replied to a request for documents that <span class="hlt">NSA</span> submitted under the Freedom of Information Act, 5 U.S.C. § 552, as implemented by the DOE in 10 C.F.R. Part 1004. This Appeal, if granted, would require that the DOE conduct another search for </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">392</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf12/poster_abs/P00177"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Spatial Hetergeneity in Mid-Summer Fluxes of Carbon, Water and Energy in Spatial Hetergeneity in Mid-Summer Fluxes of Carbon, Water and Energy in Agriculutural Plots Near the <span class="hlt">SGP</span> Central Facility Fischer, M.L.(a), Billesbach, D.(b), Berry, J.(c), Riley, W.R.(a), and Torn, M.S.(a), Lawrence Berkeley National Laboratory (a), University of Nebraska (b), Carnegie Institution of Washington (c) Twelfth Atmospheric Radiation Measurement (ARM) Science Team Meeting Patterns of land use and management are likely to dominate the spatial heterogeneity in cycles of energy, carbon, and water in ecosystems of the Southern Great Plains (<span class="hlt">SGP</span>). We report recent progress on measuring and modeling spatial heterogeneity in land surface-atmosphere exchange for different crops in the footprint of a flux system mounted on the ARM <span class="hlt">SGP</span> Central Facility 60 m tower. The first phase of our the "Portable Flux </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">393</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/data/post/14611"> <span id="translatedtitle">ARM - Data Announcements Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">New Surface Spectral Albedo VAP Provides Surface Type Observations at New Surface Spectral Albedo VAP Provides Surface Type Observations at Southern Great Plains Bookmark and Share Example quicklook from the SURFSPECALB VAP. The plot shows the estimated spectral albedo at <span class="hlt">SGP</span> for the 10-m and 25-m towers on September 11, 2004. On this day, the surface type for both towers is partial vegetation. Example quicklook from the SURFSPECALB VAP. The plot shows the estimated spectral albedo at <span class="hlt">SGP</span> for the 10-m and 25-m towers on September 11, 2004. On this day, the surface type for both towers is partial vegetation. The Surface Spectral Albedo (SURFSPECALB) value-added product (VAP) has been released for operational production at the Southern Great Plains (<span class="hlt">SGP</span>) site. This VAP creates a near-continuous best estimate of broadband and </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">394</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/extended_abs/knuteson_ro.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Progress Towards a Characterization of the Infrared Progress Towards a Characterization of the Infrared Emissivity of the Land Surface in the Vicinity of the ARM <span class="hlt">SGP</span> Central Facility: Surface (S-AERI) and Airborne Sensors (NAST-I/S-HIS) R. O. Knuteson, B. Osborne, J. Short, H. E. Revercomb, D. C. Tobin, and S. L. Nasiri University of Wisconsin, Madison Madison, Wisconsin Introduction The U.S. Department of Energy (DOE) Southern Great Plains (<span class="hlt">SGP</span>) Cloud and Radiation Testbed (CART) site provides a unique facility for the study of thermal radiation at and above the earth's surface. The site extends across a 250-km-square region in Oklahoma and Kansas dominated by rural agricultural land use. Upwelling thermal infrared (IR) radiation in the <span class="hlt">SGP</span> CART site region is strongly influenced by surface radiative properties. The surface properties most appropriate for the representa- </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">395</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/features/post/17515"> <span id="translatedtitle">ARM - Feature Stories and Releases Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">3, 2012 [Feature Stories and Releases] 3, 2012 [Feature Stories and Releases] <span class="hlt">SGP</span> Site Staff Share Successes, Challenges in the Name of Science Bookmark and Share Large-scale observation network in Korea opens door to new collaborations Daniel Hartsock and Dr. Kyungjeen Park look on as Pat Dowell describes the operation of a disdrometer at the <span class="hlt">SGP</span> site. A sensor under the instrument's 'hood' measures rain rate and drop size distribution. Daniel Hartsock and Dr. Kyungjeen Park look on as Pat Dowell describes the operation of a disdrometer at the <span class="hlt">SGP</span> site. A sensor under the instrument's 'hood' measures rain rate and drop size distribution. Dr. Kyungjeen Park, Korea Meteorological Administration, faces a tremendous responsibility: develop a microscale observing capability to support a major urban atmospheric measurement and modeling project. The project is to </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">396</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf07/extended_abs/harrison_l.pdf"> <span id="translatedtitle">Section 94</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">9 9 Shortwave Radiometry and Analysis at the Southern Great Plains (<span class="hlt">SGP</span>) Site L. Harrison, J. J. Michalsky and Q. Min Atmospheric Sciences Research Center State University of New York - Albany Albany, New York Here we report the results of three parallel efforts: the recal- 0.3%. Likewise, Joe Michalsky went to the <span class="hlt">SGP</span> site with a ibration and reanalysis of pyrano-metric data from Southern recently calibrated Eppley Normal Incidence Pyrheliometer Great Plains (<span class="hlt">SGP</span>) to improve its accuracy, use of the (NIP) and an Eppley Precision Spectral Pyranometer (PSP). multifilter rotating shadowband radiometer (MFRSR) data to derive cloud optical depths and then tests of radiative transfer The Baseline Surface Radiation Network (BSRN) and Solar models to predict shortwave irradiance under cloudy skies, </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">397</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf18/poster/P00095.pdf"> <span id="translatedtitle">PowerPoint Presentation</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Ice Storm of December 2007 at the <span class="hlt">SGP</span> Ice Storm of December 2007 at the <span class="hlt">SGP</span> Daniel Hartsock 1 , Dan J. Rusk 2 , Brad W. Orr 3 , Peter Lamb 1 1 University of Oklahoma CIMMS, 2 Cherokee Nation Industries/Atmospheric Technology Services, 3 Argonne National Laboratory 9-11 December 2007 Oklahoma and Kansas experienced a severe ice storm on December 8-11 2007 and a near miss on February 16 2008. The <span class="hlt">SGP</span>'s instrument suite can provide rare and important looks at storm evolution and can be used for forecasting and case studies. The storm's effects were widespread in Central and Eastern Oklahoma, with over 600,000 customers without power, some for weeks. Ice began in Oklahoma on the 8 th and lasted at many locations through the 10 h with ice layers that often exceeded 3/4". By contrast, the storm in February had little or no </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">398</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/extended_abs/poellot_mr.pdf"> <span id="translatedtitle">Microsoft Word - Poellot-MR.doc</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Measurements of Cloud Liquid Water Over the <span class="hlt">SGP</span> Site Measurements of Cloud Liquid Water Over the <span class="hlt">SGP</span> Site M. R. Poellot University of North Dakota Grand Forks, North Dakota R. T. Marchand Pacific Northwest National Laboratory Richland, Washington C. Twohy Oregon State University Corvallis, Oregon Introduction The University of North Dakota Citation aircraft made in situ measurements of liquid water clouds on six flights in stratus clouds during the Spring 2000 Cloud Intensive Operational Period (IOP) at the Southern Great Plains (<span class="hlt">SGP</span>) site. Four in situ instruments were used to measure cloud liquid water content (LWC): a particle measuring system (PMS) King liquid water sensor, a Counterflow Virtual Impactor (CVI), a PMS Forward Spectral Scattering Probe (FSSP) and a one-dimensional (1D) optical </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">399</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf15/poster_abs/P00130"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents: Rotating Shadowband</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Rotating Shadowband Spectroradiometer (RSS) at <span class="hlt">SGP</span>: Performance, Data Rotating Shadowband Spectroradiometer (RSS) at <span class="hlt">SGP</span>: Performance, Data Processing, and Value-Added Products Kiedron, Piotr State University of New York Albany Schlemmer, Jim The first ARM owned RSS was deployed at <span class="hlt">SGP</span> central site in May 2003. This RSS provides direct-normal, diffuse-horizontal andtotal-horizontal components of irradiance at 1001 pixels in 360nm-1050nm spectral range every minute between dawn and dusk. The instrument operated continuously since the deployment date. At first bi-weekly radiometric calibrations were instituted and upon the discovery of significant responsivity drift this rigorous calibration schedule was continued till present. However the rate of change was steadily decreasing. By September 2004 the drift was less than 1% per month. Within three month from deployment date a slight </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">400</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00100.pdf"> <span id="translatedtitle">AERONET CIMEL Data Scott M. Gianelli</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Bimodal Aerosol Size Distributions at <span class="hlt">SGP</span> Using RSS 105 and Bimodal Aerosol Size Distributions at <span class="hlt">SGP</span> Using RSS 105 and AERONET CIMEL Data Scott M. Gianelli a,b , Andrew A. Lacis b , and Barbara E. Carlson b a. Columbia University, New York, NY b. NASA Goddard Institute for Space Studies, New York, NY Abstract: Bimodal aerosol retrievals are performed on optical depth data obtained from the RSS 105 and CIMEL located at <span class="hlt">SGP</span> between 2003 and 2005, and compared to the size distribution retrievals obtained from the CIMEL data using the Dubovik and King [2000] algorithm. Significant differences in how the total aerosol optical thickness (AOT) is separated into coarse and fine modes are observed when the different algorithms are both applied to the CIMEL data, and differences in the measured optical depths between the </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_19");' href="#" title="Previous Page"> <img id="PreviousPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.previous.18x20.png" 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id="page_21" class="hiddenDiv"> <div id="header-search-bar"> <h2>Sample records for <strong>nsa sgp twp</strong> from the National Library of Energy <sup>Beta</sup> (NLE<sup>Beta</sup>)</h2> </div> <center><strong>Note: This page contains sample records for the topic "nsa sgp twp" from the National Library of Energy<sup>Beta</sup> (NLE<sup>Beta</sup>).<br> While these samples are representative of the content of NLE<sup>Beta</sup>,<br> they are not comprehensive nor are they the most current set.<br> We encourage you to perform a <a href="http://www.osti.gov/nle">real-time search of NLE<sup>Beta</sup></a><br> to obtain the most current and comprehensive results.</strong></center><p><br></p> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img 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Page" /></a> <a id="LastPageLink" onclick='return showDiv("page_25.0");' href="#" title="Last Page"> <img id="LastPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.last.18x20.png" alt="Last Page" /></a> </div> <a href="http://www.osti.gov/nle/topicpages">Index</a> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">401</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/838"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">May 15, 2006 [Facility News] May 15, 2006 [Facility News] New Micropulse Lidars to Replace Old Ones; Deployments Begin at <span class="hlt">SGP</span> Bookmark and Share A representative from Sigma Space Corporation demonstrates the operation of the new micropulse lidar to ARM instrument mentors and site operations technicians. A representative from Sigma Space Corporation demonstrates the operation of the new micropulse lidar to ARM instrument mentors and site operations technicians. On May 3, the first of seven new and upgraded micropulse lidars (MPLs) was deployed at the ARM Southern Great Plains (<span class="hlt">SGP</span>) site's Central Facility. These seven identical systems (including one spare) will replace the existing MPLs deployed at facilities throughout the <span class="hlt">SGP</span> site and include new polarization capability. The MPLs provide critical backscatter </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">402</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/443"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">30, 2007 [Facility News] 30, 2007 [Facility News] High-Speed Internet Deflects Information Overload Bookmark and Share Covering approximately 143,000 square kilometers in Oklahoma and Kansas, instruments at the various facilities throughout the <span class="hlt">SGP</span> site generate approximately 27 gigabytes of data every day. Covering approximately 143,000 square kilometers in Oklahoma and Kansas, instruments at the various facilities throughout the <span class="hlt">SGP</span> site generate approximately 27 gigabytes of data every day. A little more room in the internet link at the ARM Southern Great Plains site is providing needed relief to the crowded lines that keep data flowing from the site. In July 2007, the internet service from the <span class="hlt">SGP</span> Central Facility was switched to a higher speed (6 megabits) link, increasing the </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">403</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/1049"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Annual Quality Improvement Inspections Take Place Annual Quality Improvement Inspections Take Place Bookmark and Share During the <span class="hlt">SGP</span> site audit conducted in April 2005, a member of the Continuous Quality Improvement Program team is accompanied by a local jackrabbit at the Ringwood Extended Facility. During the <span class="hlt">SGP</span> site audit conducted in April 2005, a member of the Continuous Quality Improvement Program team is accompanied by a local jackrabbit at the Ringwood Extended Facility. The Continuous Quality Improvement Program (CQIP) implemented by the ARM Program in 1998 requires annual audits and inspection visits to each of the ARM Climate Research Facility Southern Great Plains (<span class="hlt">SGP</span>) site's 27 field facilities located in Oklahoma and Kansas. A small team of scientists and engineers conduct the inspections each year to evaluate the field </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">404</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf12/poster_abs/P00099"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Large Eddy Simulations of Fair-Weather Cumulus Case at <span class="hlt">SGP</span> Site Large Eddy Simulations of Fair-Weather Cumulus Case at <span class="hlt">SGP</span> Site Zhu, P. and Albrecht, B.A., University of Miami Twelfth Atmospheric Radiation Measurement (ARM) Science Team Meeting A fair-weather cumulus (FWC) case observed on July 6, 1997 at the ARM <span class="hlt">SGP</span> site is simulated using RAMS model. In this study, we performed a series of numerical experiments to study the basic physics underlying the FWC and the evolution of these clouds in response to the change of external forcings and conditions. The simulations indicate that the evolution of shallow cumuli is very sensitive to the initial vertical structure of moisture and the variation of the entrainment moisture fluxes. Based on the penetration theory, we are able to develop a cloud initiation parameterization using </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">405</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf14/extended_abs/zhang-gj.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">and Improving GCM Simulation of Convection and Improving GCM Simulation of Convection Using ARM Observations at the <span class="hlt">SGP</span> Site G. J. Zhang Center for Atmospheric Sciences Scripps Institution of Oceanography La Jolla, California Introduction Atmospheric convection undergoes strong diurnal variation over both land and oceans (Gray and Jacobson 1977; Dai 2001). This diurnal variation has a large impact on the atmospheric radiation budget. Convection also affects the surface energy budget by modulating the surface sensible and latent heat fluxes, in addition to solar radiation flux. Global Climate Models (GCMs) have not been very successful in simulating convection well at the <span class="hlt">SGP</span> site and elsewhere over the U.S. continent (Dai et al. 1999; Betts et al. 1999). For example, over the U.S. Southern Great Plains (<span class="hlt">SGP</span>) and the </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">406</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/data/vaps/pblht"> <span id="translatedtitle">ARM - VAP Process - pblht</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Productspblht Productspblht Documentation & Plots Technical Report Data Management Facility Plots (Quick Looks) ARM Data Discovery Browse Data Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send VAP : Planetary Boundary Layer Height (PBLHT) Instrument Categories Atmospheric Profiling Quicklook plot showing all PBL height estimates produced by the PBLHT VAP for the 05:30 UTC, April 10, 2004, radiosonde at the Southern Great Plains (<span class="hlt">SGP</span>) site. Quicklook plot showing all PBL height estimates produced by the PBLHT VAP for the 05:30 UTC, April 10, 2004, radiosonde at the Southern Great Plains (<span class="hlt">SGP</span>) site. Annual summary of PBL height estimates produced by the VAP Liu-Liang method for 2004 at <span class="hlt">SGP</span>. Annual summary of PBL height estimates produced by the VAP Liu-Liang method </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">407</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf07/extended_abs/lesht_bm.pdf"> <span id="translatedtitle">Section 15</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">An Internal Analysis of <span class="hlt">SGP</span>/CART Radiosonde An Internal Analysis of <span class="hlt">SGP</span>/CART Radiosonde Performance During the September 1996 Water Vapor Intensive Observation Period B. M. Lesht Argonne National Laboratory Argonne, Illinois Introduction The September 1996 Water Vapor Intensive Observation Per- iod (IOP) provided an excellent opportunity to investigate fur- ther the operational performance of the radiosondes used by ARM at the Southern Great Plains (<span class="hlt">SGP</span>) Cloud and Radiation Testbed (CART) site. Although many instrument inter- comparisons were conducted during the IOP, the lack of an accepted absolute standard makes evaluation of the results difficult. By focusing on information obtained from the radiosondes themselves, with minimal reference to external instruments, we hope to eliminate much of the uncertainty </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">408</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/highlights/RMTU5/view"> <span id="translatedtitle">Research Highlight</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Five-Year Statistics of Shallow Clouds at the ACRF <span class="hlt">SGP</span> Site Five-Year Statistics of Shallow Clouds at the ACRF <span class="hlt">SGP</span> Site Download a printable PDF Submitter: Berg, L., Pacific Northwest National Laboratory Kassianov, E., Pacific Northwest National Laboratory Area of Research: Cloud Distributions/Characterizations Working Group(s): Cloud Modeling Journal Reference: Berg, LK, and EI Kassianov. 2008. "Temporal variability of fair-weather cumulus statistics at the ARM <span class="hlt">SGP</span> site." Journal of Climate 21, 3344-3358. Figure 1. Five-year mean ARSCL VAP values of cloud fraction (black), cloud-base height (orange circles), cloud-top height (red), cloud thickness (blue), and cloud-chord length (green), and their average daily bias for each year (B) and low-altitude moisture (C). While fair-weather clouds (FWC) are small in size, they are ubiquitous, </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">409</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00108.pdf"> <span id="translatedtitle">Yost_ARM_Mar07.ppt</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">III. Improved Cloud Detection over the <span class="hlt">SGP</span> III. Improved Cloud Detection over the <span class="hlt">SGP</span> * GOES-8 data from June to November 1998 were reprocessed over a region within a 10-km radius of the ARM <span class="hlt">SGP</span> Central Facility using the new stats algorithm to aid cloud detection during twilight * Table 1 shows how the new VISST cloud amounts compare to 30-minute averaged cloud amounts derived from micropulse lidar (MPL) data. Values in parentheses were obtained without using the stats algorithm * An example from June 5, 1998, is illustrated in Figure 2 below * Most of the warm low clouds over Kansas and northern Oklahoma were detected by the nighttime cloud mask at 1115 Z (not shown) but missed by the twilight cloud mask at 1145 Z (Fig. 2a) * The stats algorithm restores much of the cloud cover (Fig. 2b) and this is easily verified by looking at an </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">410</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/geothermal/servlets/purl/7038730/7038730.pdf"> <span id="translatedtitle">DISCLAIMER</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary"><span class="hlt">SGP</span>-TR-- 11 5 <span class="hlt">SGP</span>-TR-- 11 5 DE88 012261 <span class="hlt">SGP</span>-TR- 1 15 A Laboratory Investigation of Steam Adsorption in Geothermal Reservoir Rocks Jeralyn Luetkehans March 1988 Financial support was provided through the Stanford Geothermal Program under Department of Energy Contract Nos. DE-AS03-80SF11459 and DE-AS07-84ID12529 and by the Dept. of Petroleum Engineering, Stanford University Stanford Geothermal Program Interdisciplinary Research in Engineering and Earth Sciences STANFORD UNIVERSITY Stanford, California DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability cr responsi- </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">411</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf16/poster_abs/P00196"> <span id="translatedtitle">W-band ARM Cloud Radar (WACR) Update and Status</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">W-band ARM Cloud Radar (WACR) Update and Status W-band ARM Cloud Radar (WACR) Update and Status PopStefanija, Ivan ProSensing, Inc. Mead, James ProSensing Inc. Widener, Kevin Pacific Northwest National Laboratory Category: Instruments Two W-band ARM Cloud Radars (WACR) have been developed for the <span class="hlt">SGP</span> and the ARM Mobile Facility (AMF) by ProSensing. The <span class="hlt">SGP</span> WACR was successfully deployed in the same shelter as the MMCR in 2005. It is currently collecting co-polarization and cross-polarization spectral moments (reflectivity, Doppler velocity, and spectral width) along with spectra data. The AMF WACR will be deployed with the AMF in Niamey, Niger early in 2006. We will present ingested WACR data formats available from the ARM Archive, a selected comparisons of WACR and MMCR data at <span class="hlt">SGP</span>, and data from </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">412</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/841"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">April 30, 2006 [Facility News] April 30, 2006 [Facility News] Disdrometer Joins Tipping Bucket to Improve Precipitation Measurements Bookmark and Share At the <span class="hlt">SGP</span> site, the disdrometer is installed near the site's main instrument cluster, approximately 50 feet east of the Central Facility. To avoid secondary splash contamination, the disdrometer's sensor cone is surrounded by splash-resistant material. At the <span class="hlt">SGP</span> site, the disdrometer is installed near the site's main instrument cluster, approximately 50 feet east of the Central Facility. To avoid secondary splash contamination, the disdrometer's sensor cone is surrounded by splash-resistant material. This spring, a pair of new distrometers began collecting data at the ARM Southern Great Plains (<span class="hlt">SGP</span>) site and the ARM Darwin site in the Tropical </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">413</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/data/post/6220"> <span id="translatedtitle">ARM - Data Announcements Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">November 12, 2009 [Data Announcements] November 12, 2009 [Data Announcements] Updated Evaluation Product Available for Calculating Surface Spectral Albedo Bookmark and Share Example of surface type estimation and high-resolution spectral albedo extrapolated from the MFR measurements at the 10-meter tower and at the 25-meter level on the 60-meter tower at the <span class="hlt">SGP</span> Central Facility. Example of surface type estimation and high-resolution spectral albedo extrapolated from the MFR measurements at the 10-meter tower and at the 25-meter level on the 60-meter tower at the <span class="hlt">SGP</span> Central Facility. An updated version of the Surface Spectral Albedo (SurfSpecAlb1Mlawer) value-added product (VAP) has been released as an Evaluation Product for the Southern Great Plains (<span class="hlt">SGP</span>) site. The original version of the algorithm </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">414</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/highlights/RMjQ5/view"> <span id="translatedtitle">Research Highlight</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Surface Summertime Radiative Forcing by Shallow Cumuli at the ARM <span class="hlt">SGP</span> Surface Summertime Radiative Forcing by Shallow Cumuli at the ARM <span class="hlt">SGP</span> Download a printable PDF Submitter: Berg, L., Pacific Northwest National Laboratory Area of Research: Radiation Processes Working Group(s): Cloud Life Cycle Journal Reference: Berg LK, EI Kassianov, CN Long, and DL Mills. 2011. "Surface summertime radiative forcing by shallow cumuli at the ARM <span class="hlt">SGP</span>." Journal of Geophysical Research - Atmospheres, 116, D01202, 10.1029/2010JD014593. Histogram of hourly average shortwave CRF (black) and longwave CRF (red) for all periods with shallow cumuli. (a) Hourly average shortwave CRF (circles), binned shortwave CRF (squares); (b) total number of hourly averages for each sky cover bin; and (c) the change in shortwave TED as a function of sky cover for all hours with </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">415</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/data/pi/25"> <span id="translatedtitle">ARM - PI Product - ARM-LBNL-NOAA Flask Sampler for Carbon Cycle Gases</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">ProductsARM-LBNL-NOAA Flask Sampler for Carbon Cycle ProductsARM-LBNL-NOAA Flask Sampler for Carbon Cycle Gases Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send PI Product : ARM-LBNL-NOAA Flask Sampler for Carbon Cycle Gases Site(s) <span class="hlt">SGP</span> General Description Data from ccg-flasks are sampled at the ARM <span class="hlt">SGP</span> site and analyzed by the NOAA Earth System Research Laboratory (ESRL) as part of the NOAA Cooperative Global Air Sampling Network. Surface samples are collected from a 60m tower at the <span class="hlt">SGP</span> Central Facility, usually once per week on one afternoon. The aircraft samples are collected approximately weekly from a chartered aircraft, and the collection flight path is centered over the tower where the surface samples are collected. Samples are collected by the ARM/LBNL Carbon Project. CO2 flask data contains measurements of CO2 </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">416</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf15/poster_abs/P00166"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents: Update on the ARM</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Update on the ARM SCM/CRM multi-year continuous forcing datasets at <span class="hlt">SGP</span> Update on the ARM SCM/CRM multi-year continuous forcing datasets at <span class="hlt">SGP</span> Xie, Shaocheng Lawrence Livermore National Laboratory Yio, John DOE/Lawrence Livermore National Laboratory Klein, Stephen Lawrence Livermore National Laboratory Cederwall, Richard Lawrence Livermore National Laboratory Statistical study of SCM/CRM simulations requires a long-term (preferably, multiyear) large-scale forcing data. The current approach to develop such multiyear datasets at <span class="hlt">SGP</span> is to use the NOAA mesoscale model RUC (Rapid Update Cycle) analyses constrained with the ARM surface and TOA measurements by using a variational analysis approach. Using this method, the LLNL ARM data infrastructure team developed a 2-year continuous forcing dataset for 1999-2000 two years ago. Since then, several ARM surface and </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">417</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf14/poster_abs/P00101"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Variability of Deep Convective Cloud Characteristics Across the <span class="hlt">TWP</span> Regime Variability of Deep Convective Cloud Characteristics Across the <span class="hlt">TWP</span> Regime Jensen, M.P.(a)(b), Del Genio, A.D.(b), Vogelmann, A.M.(c), Miller, M.A.(c), and Johnson, K.L.(c), Columbia University (a), NASA/GISS (b), Brookhaven National Laboratory (c) Deep convective clouds and their associated anvil clouds are the most obvious feature in satellite images of tropical latitudes due to their high albedo and low infrared brightness temperature.Despite the relative ease with which these cloud types are detected, the details of their radiative properties and how they are related to the hydrological and microphysical properties of the cloud system are not well understood. We present some preliminary analysis from the use of a combination of MODIS Cloud Products </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">418</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/highlights/RMTQ1/view"> <span id="translatedtitle">Research Highlight</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Cloud Regimes in the <span class="hlt">TWP</span> and Their Evolution over the MJO Cloud Regimes in the <span class="hlt">TWP</span> and Their Evolution over the MJO Download a printable PDF Submitter: Del Genio, A. D., NASA Area of Research: Cloud Distributions/Characterizations Working Group(s): Cloud Modeling Journal Reference: Chen, Y, and AD Del Genio. 2008. "Evaluation of tropical cloud regimes in observations and a general circulation model." Climate Dynamics doi:10.1007/s00382-008-0386-6. Mean highest cloud-top vertical profiles from ARSCL (solid) and ISCCP (dashed) for each ISCCP cloud regime at Manus. Relative frequency of occurrence of each cloud regime as a function of lag in pentads relative to the MJO peak for eight MJO events covering November-April of 1999-2003. Red = deep convective, orange = anvil, yellow = congestus, green = thin cirrus, blue = shallow cumulus, violet = </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">419</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00089.pdf"> <span id="translatedtitle">poster.dvi</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">POSTER POSTER #8C * ANVIL PROPERTIES OF MONSOONAL AND BREAK DEEP CONVECTION DURING <span class="hlt">TWP</span>-ICE Ann Fridlind and Andrew Ackerman * ann.fridlind@nasa.gov * NASA Goddard Institute for Space Studies, 2880 Broadway, New York, NY 10025 INTRODUCTION We aim to simulate four casees of deep convection observed during the <span class="hlt">TWP</span>-ICE IOP with a cloud-resolving model (CRM) that includes size-resolved aerosol, liquid, and ice particle types. We begin here with liquid-phase bulk micro- physics [Wyant et al., 1997]. Monsoon cases are prone to midlevel saturated layer formation due to large-scale forcings. Break (Hector) anvil fluxes are sensitive to closed versus open boundary conditions, but peak updrafts reached are not. ACKNOWLEDGMENTS * Satellite images courtesy Pat Minnis/NASA Langley * Soundings courtesy Christian Jakob/Australian BoM * Large-scale forcings courtesy Shaocheng Xie/LLNL * Surface </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">420</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/895"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">January 31, 2006 [Facility News] January 31, 2006 [Facility News] Media Day Kicks Off Tropical Cloud Study in Australia Bookmark and Share While on the ground, the Twin Otter (left) and Proteus (right) are sharing hangar space at the Royal Australian Air Force base for the duration of <span class="hlt">TWP</span>-ICE field operations. While on the ground, the Twin Otter (left) and Proteus (right) are sharing hangar space at the Royal Australian Air Force base for the duration of <span class="hlt">TWP</span>-ICE field operations. Two days after a highly successful media day, January 21 marked the official start of flight operations for the Tropical Warm Pool International Cloud Experiment in Darwin, Australia. Science team members are guiding the aircraft missions from the Bureau of Meteorology's Forecast Center in Darwin; the rest of the experiment activities are being managed </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_20");' href="#" title="Previous Page"> <img id="PreviousPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.previous.18x20.png" alt="Previous Page" /></a> <span id="PageLinks" class="pageLinks"> <span> <a 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<strong>nsa sgp twp</strong> from the National Library of Energy <sup>Beta</sup> (NLE<sup>Beta</sup>)</h2> </div> <center><strong>Note: This page contains sample records for the topic "nsa sgp twp" from the National Library of Energy<sup>Beta</sup> (NLE<sup>Beta</sup>).<br> While these samples are representative of the content of NLE<sup>Beta</sup>,<br> they are not comprehensive nor are they the most current set.<br> We encourage you to perform a <a href="http://www.osti.gov/nle">real-time search of NLE<sup>Beta</sup></a><br> to obtain the most current and comprehensive results.</strong></center><p><br></p> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" 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class="hlt">TWP</span> ARM Site Kollias, P., Albrecht B.A., and Dow B.J., University of Miami Eleventh Atmospheric Radiation Measurement (ARM) Science Team Meeting Fair-weather cumuli are fundamental in regulating the vertical structure of water vapor and entropy in the lowest 2 km of the Earth's atmosphere over vast areas of the oceans. Using data from the mm-wavelength cloud radar, the micro-pulse lidar and ceilometer at the Nauru (<span class="hlt">TWP</span>-ARM) site, a statistical description of the field of fair weather cumulus is inferred. Frequency diagrams of cloud thickness, fractional coverage, updraft-downdraft magnitudes and cloud reflectivity are calculated. The relationship of the statistical behavior of the cumulus field to the </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">422</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/meetings/2009/presentations/0331/16_Varble.pdf"> <span id="translatedtitle">Preliminary Differences Between CPOL and CRM</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">differences between <span class="hlt">TWP</span>-ICE data differences between <span class="hlt">TWP</span>-ICE data from the CPOL radar and the CRM: Should we point fingers at convective intensity, microphysics, or both? Adam Varble 1 , Ed Zipser 1 , and Ann Fridland 2 1 University of Utah 2 NASA Goddard Institute for Space Studies Outline * CRM vs. CPOL - Constant altitude radar reflectivity histograms * Active Period Examples * Suppressed Period Example - Horizontal and vertical radar reflectivity cross sections * Active Period Examples * Suppressed Period Example * Preliminary Conclusions Histograms (Active) Cross-Sections - Active (Baseline) 6 Hours Later... Cross-Sections - Active (Sensitivity) 6 Hours Later... Stratiform Differences Histograms (Suppressed) Cross-Sections - Suppressed Preliminary Conclusions * Active Period - Both CRM runs produce too much convective area </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">423</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf07/extended_abs/petch_jc.pdf"> <span id="translatedtitle">Section 65</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Investigating Cloud Radiative Forcing in the Tropical Investigating Cloud Radiative Forcing in the Tropical West Pacific Using a Single-Column Model J. C. Petch and J. T. Kiehl National Center for Atmospheric Research Boulder, Colorado Introduction The Tropical Western Pacific (<span class="hlt">TWP</span>) is an important region for world climate (Webster and Lucas 1992) and was the subject of the Tropical Ocean Global Atmosphere-Coupled Ocean Atmosphere Response Experiment (TOGA-COARE) in 1992/3. This experiment included an intensive observational period (IOP) from November 1992 through March 1993, which provided observations suitable for creat- ing datasets that can be used for forcing either single-column models (SCMs) or cloud-resolving models (CRMs). Organized cloud systems in the <span class="hlt">TWP</span> have a major impact on radiation. The accurate representation of these cloud systems </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">424</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf12/poster_abs/P00007"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">A Climatology of Cloud & Radiative Properties Derived from GMS-5 Data Over A Climatology of Cloud & Radiative Properties Derived from GMS-5 Data Over the Tropical Western Pacific Nordeen, M.L.(a), Doelling, D.R.(a), Khaiyer, M.M.(a), Rapp, A.D.(a), and Minnis, P.(b), Analytical Services & Materials, Inc. (a), National Aeronautics and Space Administration-Langley Research Center (b) Twelfth Atmospheric Radiation Measurement (ARM) Science Team Meeting Satellite derived cloud and radiative properties can provide continuous spatial and temporal coverage over the Tropical Western Pacific (<span class="hlt">TWP</span>). The <span class="hlt">TWP</span> is an area with few meteorological stations, but is an interesting region in global climate studies. Starting with the Nauru99 Intensive Operational Period (IOP) (June-July 1999), two years of hourly Geostationary Meteorological Satellite (GSM-5) images are used in the </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">425</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf13/poster_abs/P00191"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Boundary Layer Structure and Fair-Weather Cumulus Characteristics at the Boundary Layer Structure and Fair-Weather Cumulus Characteristics at the <span class="hlt">TWP</span> ARM Site - Comparisons with Other Tropical and Subtropical Sites Albrecht, B. and Kollias, P., University of Miami Thirteenth Atmospheric Radiation Measurement (ARM) Science Team Meeting Fair-weather cumuli are fundamental in regulating the vertical structure of water vapor and entropy in the lowest 2 km of the Earths atmosphere over vast areas of the oceans. Boundary layer structures and cloud characteristics observed at Nauru (ARM <span class="hlt">TWP</span>) during suppressed convective conditions are compared with those observed at other tropical and subtropical sites. Over three years of data from the mm-wavelength cloud radar and ceilometer observations at the Nauru site are analyzed and a statistical description of the field of fair weather cumulus is inferred. </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">426</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf08/extended_abs/spinhirne_jd.pdf"> <span id="translatedtitle">spinhirne-98.pdf</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">1 1 Optical Properties of the 1997 Smoke Event at the ARM Tropical Western Pacific Site J. D. Spinhirne NASA-Goddard Space Flight Center Laboratory of Atmospheres Greenbelt, Maryland D. L. Hlavka and J. R. Campbell Science Systems and Applications Inc. NASA-Goddard Space Flight Center Greenbelt, Maryland C. J. Flynn Pacific Northwest National Laboratory Richland, Washington Introduction Drought conditions and population pressures in Indonesia and surrounding areas in the Tropical Western Pacific (<span class="hlt">TWP</span>) sparked massive biomass burning episodes during September-November of 1997. Some of this smoke advected over the Manus Island Atmospheric Radiation Measurement (ARM) <span class="hlt">TWP</span> site. Analysis of smoke-related aerosol is of interest. Smoke aerosol from biomass burning is thought to be a major source of absorbing aerosol in the </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">427</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf16/extended_abs/mcfarquhar_g.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Horizontal and Vertical Profiles of In-Situ Cloud Horizontal and Vertical Profiles of In-Situ Cloud Properties Measured During Tropical Warm Pool International Cloud Experiment G. McFarquhar, M. Freer, and J. Um University of Illinois at Urbana-Champaign Urbana, Illinois G. Kok Droplet Measurement Technologies Boulder, Colorado R. McCoy and T. Tooman Sandia National Laboratories Livermore, California J. Mace University of Utah Salt Lake City, Utah Introduction In-situ measurements of ice particle sizes, shapes and numbers were made in fresh anvils, aging anvils and in generic cirrus during <span class="hlt">TWP</span>-ICE. The vertical profiles and horizontal profiles performed by the Scaled Composites Proteus aircraft were made on 7 different days as illustrated in Table 1. Table 1. Summary of flights conducted during <span class="hlt">TWP</span>-ICE; *designates that spiral was conducted over Darwin, </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">428</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf07/extended_abs/clements_we.pdf"> <span id="translatedtitle">Section 113</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">0°S 0°S 10°N 135°E 150°W Session Papers (a) Mail Stop D407, P.O. Box 1663, 505-667-1186, twppo@lanl.gov. 513 Figure 1. Equatorial Western Pacific region showing <span class="hlt">TWP</span> locale (dashed area) and proposed Atmospheric and Radiation Cloud Station (ARCS) sites (circles). Tropical Western Pacific Program: Status Report W. E. Clements and F. J. Barnes Tropical Western Pacific Program Office (a) University of California, Los Alamos National Laboratory Los Alamos, New Mexico Introduction The Tropical Western Pacific (<span class="hlt">TWP</span>) locale is the second Cloud and Radiation Testbed (CART) locale to be imple- mented by the Atmospheric Radiation Measurement (ARM) Program. It is a large expanse of tropical ocean and maritime continent lying roughly between and latitude and from to longitude (Figure 1). The maritime </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">429</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf10/extended_abs/austin_rt.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">LIRAD Analysis of <span class="hlt">TWP</span> Cirrus at Nauru LIRAD Analysis of <span class="hlt">TWP</span> Cirrus at Nauru R. T. Austin, C. Mitrescu, and G. L. Stephens Department of Atmospheric Science Colorado State University Fort Collins, Colorado Introduction The purpose of this work is to implement algorithms for retrieval of high-cloud emittance and optical depth using lidar-radiometer (LIRAD) analysis based on available continuous data streams from the Atmospheric Radiation Measurement (ARM) Program's Cloud and Radiation Testbed (CART) sites. Routine, continuous operation of the micropulse lidar (MPL), infrared thermometer (IRT), microwave radiometer (MWR), and frequent sonde soundings should allow for near-continuous retrieval of LIRAD products, subject to time and accuracy limitations described later in this paper. Initial development of </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">430</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/site_reports/twp/arm-00-005.pdf"> <span id="translatedtitle">Tropical Western Pacific</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">ARM-00-005 ARM-00-005 RPT(<span class="hlt">TWP</span>)-010.006 LA-UR-004434 Tropical Western Pacific Site Science Mission Plan July - December 2000 Prepared for the U.S. Department of Energy under Contract W-7405-ENG-36 Tropical Western Pacific Project Office Atmospheric and Climate Sciences Group (EES-8) Earth and Environmental Sciences Division Los Alamos National Laboratory Los Alamos, NM 87545 This report and previous versions are available electronically at the following web sites: http://www.arm.gov/docs/sites/<span class="hlt">twp</span>/science_plan/archive.html http://www.twppo.lanl.gov/docs/office.html 2 DISCLAIMER This report was prepared as an account of work sponsored by the United States Government. Neither the United States nor an agency thereof, nor any of their employees, makes any warranty, expresses or </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">431</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/instruments/gms"> <span id="translatedtitle">ARM - Instrument - gms</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">govInstrumentsgms govInstrumentsgms Documentation GMS : XDC documentation ARM Data Discovery Browse Data Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Instrument : Geostationary Meteorological Satellite (GMS) Note: gms is currently inactive and/or retired. Active Dates 1996.10.01 - 2003.02.16 Instrument Categories Satellite Observations <!-- Picture of the GMS Picture of the GMS --> General Overview GMS-5 satellite images are taken over the Tropical Western Pacific (<span class="hlt">TWP</span>), over each of the <span class="hlt">TWP</span> sites. The raw data are downlinked to the SeaSpace Corp. receiving station at the University of Hawaii. The GMS-5 was launched in March 1995 into a geostationary orbit above 0°N, 140°E. It carries a Visible and Infrared Spin Scan Radiometer (VISSR) with four channels, one </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">432</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/meetings/2006/posters/06awards/schumacher.pdf"> <span id="translatedtitle">Courtney Schumacher Courtney Schumacher</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Courtney Schumacher Courtney Schumacher Courtney Schumacher 1 1 , Robert Houze , Robert Houze 2 2 , Peter May , Peter May 3 3 , Kaycee Frederick , Kaycee Frederick 1 1 , Jasmine Cetrone , Jasmine Cetrone 2 2 , and Andreas Vallgren , and Andreas Vallgren 3 3 1 1 Texas A&M University, Texas A&M University, 2 2 University of Washington, University of Washington, 3 3 Bureau of Meteorology Research Centre Bureau of Meteorology Research Centre Vertical Echo Distribution Rain (∆X C and ∆X S ) and Anvil (∆X A ) Area Rainfall (R c and R s ) This study focuses on the composite water budget of tropical convective systems observed during the Tropical Warm Pool- Ice Cloud Experiment (<span class="hlt">TWP</span>-ICE) in January - February 2006. <span class="hlt">TWP</span>-ICE EXAMPLE CASE ACKNOWLEDGEMENTS: We'd like to thank Stacy Brodzik for her invaluable efforts in </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">433</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf10/extended_abs/clements_we.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Western Pacific 2000 Western Pacific 2000 W. E. Clements, F. J. Barnes, L. Jones, and A. Haruta University of California Los Alamos National Laboratory Los Alamos, New Mexico M. Ivey Sandia National Laboratories Albuquerque, New Mexico P. Lefale South Pacific Regional Environment Programme Apia, Samoa Introduction The Atmospheric Radiation Measurement (ARM) Program's Tropical Western Pacific (<span class="hlt">TWP</span>) Program is currently operating two Atmospheric Radiation and Cloud Stations (ARCS) in the <span class="hlt">TWP</span> locale. The first ARCS site was installed on Los Negros Island in Manus Province, Papua New Guinea (PNG), in October 1996. The Tropical Western Pacific Program Office (TWPPO) and the PNG National Weather Service (NWS) have collaborated in operating the Manus site since its installation. Located on Nauru </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">434</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf05/extended_abs/barr_sa.pdf"> <span id="translatedtitle">X:\ARM_19~1\PGS19-27.WPD</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">~11µm) ~11µm) T b 2.1 S, T b <273 K, 220 K < T b <273 K, T b <220 K 147 E Session Papers 19 Evidence for Island Effects and Diurnal Signals in Satellite Images of Clouds Over the Tropical Western Pacific S. A. Barr-Kumarakulasinghe Marine Sciences Research Center State University of New York Stony Brook, New York R. M. Reynolds and P. J. Minnett Oceanographic and Atmospheric Sciences Division Brookhaven National Laboratory Upton, New York Introduction Instruments to measure atmospheric radiation and ancillary meteorological variables will be set up on Manus Island as the first site of the tropical western pacific (<span class="hlt">TWP</span>) locale of the Atmospheric Radiation Measurements (ARM) program. Manus is in the "warm pool" region of the <span class="hlt">TWP</span>. This region is critical in establishing global atmospheric </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">435</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/1111"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Scientists Convene in Australia to Plan International Cloud Experiment Scientists Convene in Australia to Plan International Cloud Experiment Bookmark and Share During <span class="hlt">TWP</span>-ICE, cloud property data will be obtained from numerous research aircraft and a network of surface-based remote sensing sites, including a ship operating in the Timor Sea and numerous ground sites in a 200 km diameter around the ARM Climate Research Facility site in Darwin, Australia. During <span class="hlt">TWP</span>-ICE, cloud property data will be obtained from numerous research aircraft and a network of surface-based remote sensing sites, including a ship operating in the Timor Sea and numerous ground sites in a 200 km diameter around the ARM Climate Research Facility site in Darwin, Australia. Coming from as far away as Italy, Switzerland, and the United States, a 45 member team gathered in Darwin, Australia, in mid-November to discuss plans </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">436</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf08/extended_abs/white_ab.pdf"> <span id="translatedtitle">white-98.pdf</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">5 5 A Comparison of Shipboard and Island Observations from the Combined Sensor Program A. B. White Cooperative Institute for Research in Environmental Sciences University of Colorado NOAA-Environmental Technology Laboratory Boulder, Colorado C. W. Fairall and M. J. Post NOAA-Environmental Technology Laboratory Boulder, Colorado Introduction Two issues concerning the Tropical Western Pacific (<span class="hlt">TWP</span>) Atmospheric Radiation and Cloud Stations (ARCS) are these: To what degree are the measurements obtained from the island ARCS influenced by the islands themselves? What is the spatial representativeness of measurements from individual ARCS in the <span class="hlt">TWP</span> region? The 1996 Combined Sensor Program (CSP) (Post et al. 1997) gave an opportunity to address these questions by providing </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">437</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf09/poster_abs/P00045"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Initial Cloud Properties Derived from GMS Over the Tropical Western Pacific Initial Cloud Properties Derived from GMS Over the Tropical Western Pacific Doelling, D.R., Ho, S.-P., Smith, W.L., Jr., Analytical Services and Materials, Inc.; Minnis, P., National Aeronautics and Space Administration-Langley Research Center Ninth Atmospheric Radiation Measurement (ARM) Science Team Meeting Satellite data are needed to provide measurements of the earth-atmosphere shortwave (SW) albedo, outgoing longwave radiation (OLR), and cloud and surface radiative properties for the Atmospheric Radiation Measurement (ARM) Program's Tropical Western Pacific (<span class="hlt">TWP</span>) domain. Geostationary Meteorological Satellite (GMS) data have been archived since November 1996 and provide the basis for monitoring these essential parameters over the ARM <span class="hlt">TWP</span>. This paper describes the initial efforts and results of developing </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">438</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/897387"> <span id="translatedtitle">Experiment to Characterize Tropical Cloud Systems</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">A major experiment to study tropical convective cloud systems and their impacts will take place around Darwin, Northern Australia in early 2006. The Tropical Warm Pool International Cloud Experiment (<span class="hlt">TWP</span>-ICE) is a collaboration including the DOE ARM (Atmospheric Radiation Measurement) and ARM-UAV programs, NASA centers, the Australian Bureau of Meteorology, CSIRO, and universities in the USA, Australia, Japan, the UK, and Canada. <span class="hlt">TWP</span>-ICE will be preceded in November/December 2004 by a collaborating European aircraft campaign involving the EU SCOUT-O3 and UK NERC ACTIVE projects. Detailed atmospheric measurements will be made in the Darwin area through the whole Austral summer, giving unprecedented coverage through the pre-monsoon and monsoon periods.</p> <div class="credits"> <p class="dwt_author">May, Peter T.; Mather, Jim H.; Jakob, Christian</p> <p class="dwt_publisher"></p> <p class="publishDate">2005-08-02T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">439</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00012.pdf"> <span id="translatedtitle">Microsoft PowerPoint - UM_ARM2007_eps.ppt</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Scattering Scattering Properties of Aggregates of Plates from <span class="hlt">TWP</span>-ICE Junshik Um and Greg M. McFarquhar University of Illinois, Urbana IL junum@atmos.uiuc.edu 1. Introduction During the 2006 Tropical Warm Pool International Cloud Experiment (<span class="hlt">TWP</span>-ICE), aggregates of bullet rosettes (Um and McFarquhar 2007) and chain aggregates of plates were observed using a Cloud Particle Imager (CPI). Aggregates of plates were also observed during previous field campaigns (i.e., TEFLUN-B, CRYSTAL-FACE, and EMERALD-II). Many aggregates consisted of clusters of 2 or more plates attached together. Here the single-scattering properties (i.e., asymmetry parameter g and scattering phase function P 11 ) for idealized models describing these aggregates are calculated using a ray-tracing code at solar wavelength (λ=0.55μm). The relation </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">440</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/extended_abs/nordeen_ml.pdf"> <span id="translatedtitle">Nordeen-ML</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">GMS-5 Satellite-Derived Cloud Properties Over the GMS-5 Satellite-Derived Cloud Properties Over the Tropical Western Pacific M. L. Nordeen, D. R. Doelling, M. M. Khaiyer, and A. D. Rapp Analytical Service and Materials, Inc. Hampton, Virginia P. Minnis and L. Nguyen Atmospheric Sciences Division National Aeronautics and Space Administration Langley Research Center Hampton, Virginia Introduction Satellite monitoring is used to supplement the paucity of surface data in the Tropical Western Pacific (<span class="hlt">TWP</span>). By using satellite data, cloud properties and top-of-atmosphere broadband radiative fluxes can be derived and used for a variety of applications. In turn, these products may be used to develop a climatological base for the <span class="hlt">TWP</span>. The focus of this study is to produce satellite-derived cloud properties </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_21");' href="#" title="Previous Page"> <img id="PreviousPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.previous.18x20.png" alt="Previous Page" /></a> <span id="PageLinks" class="pageLinks"> <span> <a onClick='return showDiv("page_1");' href="#">1</a> <a onClick='return showDiv("page_2");' 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(NLE<sup>Beta</sup>)</h2> </div> <center><strong>Note: This page contains sample records for the topic "nsa sgp twp" from the National Library of Energy<sup>Beta</sup> (NLE<sup>Beta</sup>).<br> While these samples are representative of the content of NLE<sup>Beta</sup>,<br> they are not comprehensive nor are they the most current set.<br> We encourage you to perform a <a href="http://www.osti.gov/nle">real-time search of NLE<sup>Beta</sup></a><br> to obtain the most current and comprehensive results.</strong></center><p><br></p> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_22");' 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src="http://www.osti.gov/nlesearch/images/icon.last.18x20.png" alt="Last Page" /></a> </div> <a href="http://www.osti.gov/nle/topicpages">Index</a> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">441</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf14/extended_abs/kollias-p.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Boundary Layer Cloud Climatology at the ARM <span class="hlt">TWP</span> Nauru Boundary Layer Cloud Climatology at the ARM <span class="hlt">TWP</span> Nauru Site P. Kollias Cooperative Institute for Research in Environmental Science/ Environmental Technology Laboratory University of Colorado Boulder, Colorado B.A. Albrecht University of Miami Miami, Florida Introduction Boundary layer (BL) clouds are fundamental in regulating the vertical structure of water vapor and entropy in the lowest 2 km of the Earth's atmosphere. Data on fair-weather cumuli have also received relatively little recent attention compared with marine stratocumulus clouds. Studies made thirty years ago, Barbados Oceanographic and Meteorological Experiment (BOMEX, 1969) and the Atlantic Trade- Wind Experiment (ATEX, 1969), provided key analyses (Augstein et al., 1973; Holland and Rassmusen, </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">442</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/data/post/18123"> <span id="translatedtitle">ARM - Data Announcements Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">New Evaluation Product Provides Thermodynamic Variables from Multiple New Evaluation Product Provides Thermodynamic Variables from Multiple Instruments Bookmark and Share INTERPSONDE output from the <span class="hlt">SGP</span> Central Facility during the Midlatitude Continental Convective Clouds Experiment from April 26, 2011. INTERPSONDE output from the <span class="hlt">SGP</span> Central Facility during the Midlatitude Continental Convective Clouds Experiment from April 26, 2011. The Interpolated Sonde (INTERPSONDE) value-added product (VAP) is an intermediate step of the MERGESONDE VAP that produces a daily file of atmospheric state variables (temperature, humidity, pressure, and winds) from radiosonde soundings, the microwave radiometer, and surface meteorological instruments. INTERPSONDE includes many of the same sophisticated scaling/interpolation/smoothing schemes that are the hallmark </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">443</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf10/extended_abs/ferrare_ra.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Characterization of the Atmospheric State above the <span class="hlt">SGP</span> Characterization of the Atmospheric State above the <span class="hlt">SGP</span> Using Raman Lidar and AERI/GOES Measurements R. A. Ferrare National Aeronautics and Space Administration Langley Research Center Hampton, Virginia D. D. Turner Pacific Northwest National Laboratory Richland, Washington L. A. Heilman Science Applications International Corporation National Aeronautics and Space Administration Langley Research Center Hampton, Virginia W. F. Feltz University of Wisconsin Madison, Wisconsin T. P. Tooman Sandia National Laboratories Livermore, California O. Dubovik Science Systems and Applications, Inc. National Aeronautics and Space Administration Goddard Space Flight Center Greenbelt, Maryland R. N. Halthore Brookhaven National Laboratory Upton, New York </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">444</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf12/extended_abs/majurec-n.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Automated W-Bands/S-Band Radar Profilers Automated W-Bands/S-Band Radar Profilers for the ARM <span class="hlt">SGP</span> 2001 N. Majurec, A. Khandwalla, and S. M. Sekelsky University of Massachusetts Amherst, Massachusetts L. Li National Aeronautics and Space Administration Goddard Space Flight Center Greenbelt, Maryland C. R. Williams and K. S. Gage National Oceanic and Atmospheric Administration Aeronomy Laboratory Boulder, Colorado Abstract The University of Massachusetts (UMass) and National Oceanic and Atmospheric Administration (NOAA) Aeronomy Laboratory deployed automated vertically profiling radar systems at the U.S. Department of Energy (DOE) Atmospheric Radiation Measurement (ARM) Program Southern Great Plains (<span class="hlt">SGP</span>) Cloud and Radiation Testbed (CART) facility in Oklahoma for an extended </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">445</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/programdocs/doe-sc-arm-0505.pdf"> <span id="translatedtitle">Executive Summary</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">5 5 Nauru Island Effect Study (NIES) IOP Science Plan June 2001 Chuck Long Pacific Northwest National Laboratory ARM <span class="hlt">TWP</span> Site Scientist, NIES IOP Lead Scientist Richland, Washington Work supported by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research C. Long., DOE/SC-ARM-0505 Contents 1. Background ............................................................................................................................... 1 2. Scientific Requirement.............................................................................................................. 5 3. Experimental Approach ............................................................................................................ </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">446</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/4027792"> <span id="translatedtitle">PROCEEDINGS OF THE CONFERENCE ON BREEDING, ECONOMICS AND SAFETY IN LARGE FAST POWER REACTORS, OCTOBER 7-10, 1963</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">Nuclear data, reactivity coefficients, core meltdown and the maximum accident, performance, fuels, economics, safety, Doppler effect theory, and Doppler experiments are discussed for fast power breeder reactors. Separate abstracts are prepared for 22 of the 46 papers presented. The remaining papers were previously abstracted in <span class="hlt">NSA</span></p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate">1963-12-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">447</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/21371107"> <span id="translatedtitle">Interface width effect on the classical Rayleigh-Taylor instability in the weakly nonlinear regime</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">In this paper, the interface width effects (i.e., the density gradient effects or the density transition layer effects) on the Rayleigh-Taylor instability (RTI) in the weakly nonlinear (WN) regime are investigated by numerical simulation (NS). It is found that the interface width effects dramatically influence the linear growth rate in the linear growth regime and the mode coupling process in the WN growth regime. First, the interface width effects decrease the linear growth rate of the RTI, particularly for the short perturbation wavelengths. Second, the interface width effects suppress (reduce) the third-order feedback to the fundamental mode, which induces the nonlinear saturation amplitude (<span class="hlt">NSA</span>) to exceed the classical prediction, 0.1lambda. The wider the density transition layer is, the larger the <span class="hlt">NSA</span> is. The <span class="hlt">NSA</span> in our NS can reach a half of its perturbation wavelength. Finally, the interface width effects suppress the generation and the growth of the second and the third harmonics. The ability to suppress the harmonics' growth increases with the interface width but decreases with the perturbation wavelength. On the whole, in the WN regime, the interface width effects stabilize the RTI, except for an enhancement of the <span class="hlt">NSA</span>, which is expected to improve the understanding of the formation mechanism for the astrophysical jets, and for the jetlike long spikes in the high energy density physics.</p> <div class="credits"> <p class="dwt_author">Wang, L. F. [LCP, Institute of Applied Physics and Computational Mathematics, Beijing 100088 (China); State Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Beijing 100083 (China); Ye, W. H. [LCP, Institute of Applied Physics and Computational Mathematics, Beijing 100088 (China); Department of Physics, Zhejiang University, Hangzhou 310027, China and CAPT, Peking University, Beijing 100871 (China); Li, Y. J. [State Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Beijing 100083 (China)</p> <p class="dwt_publisher"></p> <p class="publishDate">2010-05-15T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">448</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/4112071"> <span id="translatedtitle">PROCEEDINGS OF AEROSPACE NUCLEAR SAFETY, OCTOBER 1-4, 1963, ALBUQUERQUE, NEW MEXICO</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">Separate abstracts were prepared for 18 of the 28 papers presented; 8 were previously abstracted in <span class="hlt">NSA</span>. Topics covered include safety programs and philosophy, nuclear safety aspects of SNAP desigu and of propulsion reactor design, environmental factors, and re-entry and postmission disposal. (R.E.U.)</p> <div class="credits"> <p class="dwt_author">Dunlap, R.E. ed.</p> <p class="dwt_publisher"></p> <p class="publishDate">1964-10-31T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">449</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/4695660"> <span id="translatedtitle">THE BERKELEY HIGH-ENERGY PHYSICS STUDY AT THE ERNEST O. LAWRENCE RADIATION LABORATORY, BERKELEY, CALIFORNIA, JUNE 15 THROUGH AUGUST 15, 1961</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">Seminar talks and special reports presented by the Berkeley summer study group are compiled. Included in the compilation are 24 seminar talks, 10 reports, a summary of theoretical conclusions, and comments on experimental questions. Separate abstracts have been prepared for 18 seminar talks and all of the reports. Five seminar talks have been abstracted previously in <span class="hlt">NSA</span>. (M.P.G.)</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate">1963-10-31T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">450</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://spaf.cerias.purdue.edu/usgov/commerce.pdf"> <span id="translatedtitle">Testimony before the Senate Committee on Commerce, Science, and Transportation</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">as an advisor to Federal law enforcement and defense agencies, in- cluding the FBI, the Air Force and the <span class="hlt">NSA</span>. I also the chair of USACM, the U.S. public policy committee of the ACM. With over 90,000 members, ACM point for ACM's interaction with the U.S. Congress and government organizations. It seeks to educate</p> <div class="credits"> <p class="dwt_author">Holland, Jeffrey</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">451</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/4054962"> <span id="translatedtitle">PROCEEDINGS OF THE US/UK MEETING ON THE COMPATIBILITY PROBLEMS OF GAS- COOLED REACTORS HELD AT OAK RIDGE NATIONAL LABORATORY, FEBRUARY 24-26, 1960</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">Forty papers presented at the US/UK Meeting on the Compatibility Problems of Gas Cooled Reactors are given. Thirty-two of the papers are covered by separate abstracts. Eight papers were previously abstracted for <span class="hlt">NSA</span>. (M.C.G.)</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate">1961-03-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">452</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://journals.ametsoc.org/doi/pdf/10.1175/1520-0442%282003%29016%3C0445%3AASCPAR%3E2.0.CO%3B2"> <span id="translatedtitle">Arctic Stratus Cloud Properties and Radiative Forcing Derived from Ground-Based Data Collected at Barrow, Alaska</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">A record of single-layer and overcast low-level Arctic stratus cloud properties has been generated using data collected from May to September 2000 at the Atmospheric Radiation Measurement (ARM) North Slope of Alaska (<span class="hlt">NSA</span>) (71.3N, 156.6W) site ...</p> <div class="credits"> <p class="dwt_author">Xiquan Dong; Gerald G. Mace</p> <p class="dwt_publisher"></p> <p class="publishDate">2003-02-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">453</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf18/poster/P00114.pdf"> <span id="translatedtitle">Microsoft PowerPoint - ARM2008_poster_mbc_raf [Compatibility Mode]</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">l l d W t V V i bilit N Cl d M d Aerosol and Water Vapor Variability Near Clouds Measured Aerosol and Water Vapor Variability Near Clouds Measured Aerosol and Water Vapor Variability Near Clouds Measured p y b h U d d <span class="hlt">SGP</span> R Lid by the Upgraded <span class="hlt">SGP</span> Raman Lidar by the Upgraded <span class="hlt">SGP</span> Raman Lidar by the Upgraded <span class="hlt">SGP</span> Raman Lidar by t e Upg aded SG a a da 1 2 3 4 4 Richard Ferrare 1 David Turner 2 Marian Clayton 3 Rob Newsom 4 Chitra Sivaraman 4 Richard Ferrare 1 David Turner 2 Marian Clayton 3 Rob Newsom 4 Chitra Sivaraman 4 Richard Ferrare , David Turner , Marian Clayton , Rob Newsom , Chitra Sivaraman 1 NASA L l R h C t 2 U i it f Wi i M di 3 S i S t d A li ti I 4 P ifi N th t N ti l L b t 1 NASA Langley Research Center 2 University of Wisconsin-Madison 3 Science Systems and Applications Inc 4 Pacific Northwest National Laboratory NASA Langley Research Center University of Wisconsin Madison Science Systems and Applications, Inc. </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">454</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/meetings/2008/presentations/0310/5_Matrosov_Deep_Convection.pdf"> <span id="translatedtitle">Slide 1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">WSR-88D profiles over <span class="hlt">SGP</span> ARM site WSR-88D profiles over <span class="hlt">SGP</span> ARM site PI VAP (X. Dong et al., University of North Dakota) Examples from X. Dong: a) MMCR time-height cross-section b) KVNX time-height cross section c) merged product d) surface rain rate and LWP -40 -30 -20 -10 0 10 20 30 40 0 1 2 3 4 5 6 7 8 9 10 11 12 observed reflectivity, Z e (dBZ) height AGL (km) MMCR general mode 1-May-2007 black lines - 10:00 UTC blue lines - 12:00 UTC KVNX A stratiform precipitation case study at <span class="hlt">SGP</span> (1 May 2007) -40 -30 -20 -10 0 10 20 30 40 0 1 2 3 4 5 6 7 8 9 10 11 12 observed reflectivity, Z e (dBZ) height AGL (km) MMCR general mode 1-May-2007 black lines - 10:00 UTC blue lines - 12:00 UTC KVNX 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 0 5 10 15 20 25 30 35 40 45 time (UTC, decimal) reflectivity (dBZ) KVNX measured at 1.66 km AGL over <span class="hlt">SGP</span> S-band calculated from JWD DSDs 1 May 2007 Comparisons of KVNX and S-band JWD reflectivities </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">455</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/dataexplorer/details.jsp?id=1077769"> <span id="translatedtitle">ARM's Broadband Radiometer Station (BRS) Data</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/dataexplorer/">DOE Data Explorer (OSTI) </a></p> <p class="result-summary">ARM's BRS data contains measurements of broadband shortwave and longwave, downwelling, upwelling, and normal radiation. The Broadband Radiometer Station (BRS) has collected data since 2001. Data Plots can be viewed for the BRS datastream through ARM's Thumbnail Browser. The primary site for BRS data collection is the Southern Great Plains (<span class="hlt">SGP</span>).</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">456</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://pangea.stanford.edu/ERE/pdf/IGAstandard/SGW/2009/lei.pdf"> <span id="translatedtitle">PROCEEDINGS, Thirty-Fourth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 9-11, 2009</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">, Stanford, California, February 9-11, 2009 <span class="hlt">SGP</span>-TR-187 DISTRICT HEATING MODELLING AND SIMULATION Lei Haiyan1 air pollution and save conventional energy, geothermal energy as a heat source for district heating. This paper describes the geothermal resource and district heating system in Tianjin. Heat load for one sample</p> <div class="credits"> <p class="dwt_author">Stanford University</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">457</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://pangea.stanford.edu/ERE/pdf/IGAstandard/SGW/2010/williams.pdf"> <span id="translatedtitle">PROCEEDINGS, Thirty-Fifth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 1-3, 2010</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">, Stanford, California, February 1-3, 2010 <span class="hlt">SGP</span>-TR-188 THERMAL ENERGY RECOVERY FROM ENHANCED GEOTHERMAL to the thermal energy contained in the fractured volume comprising the reservoir. One approach to EGS resource crustal heat flow is most favorable for EGS development (Figure 1), were included in the recent USGS</p> <div class="credits"> <p class="dwt_author">Stanford University</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">458</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://pangea.stanford.edu/ERE/research/geoth/publications/techreports/SGP-TR-177.pdf"> <span id="translatedtitle">Liquid-Gas Relative Permeabilities in Fractures: Effects of Flow Structures, Phase Transformation and Surface</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary"><span class="hlt">SGP</span>-TR-177 Liquid-Gas Relative Permeabilities in Fractures: Effects of Flow Structures, Phase) the liquid-gas relative permeabilities in fractures can be modeled by characterizing the flow structures permeabilities in both smooth and rough fractures. For the theoretical analysis of liquid-vapor relative</p> <div class="credits"> <p class="dwt_author">Stanford University</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">459</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://pangea.stanford.edu/ERE/pdf/IGAstandard/SGW/2011/oka.pdf"> <span id="translatedtitle">PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 31 -February 2, 2011</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 31 - February 2, 2011 <span class="hlt">SGP</span>-TR-191 GEOTHERMAL FLUID FLOW MONITORING BY THE REPEAT GRAVITY MEASUREMENT AT THE TAKIGAMI GEOTHERMAL FIELD, JAPAN -APPLICATION OF HYBRID GRAVITY</p> <div class="credits"> <p class="dwt_author">Stanford University</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">460</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://pangea.stanford.edu/ERE/pdf/IGAstandard/SGW/2011/satman.pdf"> <span id="translatedtitle">PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 31 -February 2, 2011</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 31 - February 2, 2011 <span class="hlt">SGP</span>-TR-191 SUSTAINABILITY OF GEOTHERMAL DOUBLETS-in the natural energy flow will slowly replenish the geothermal system and it will again be available</p> <div class="credits"> <p class="dwt_author">Stanford University</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_22");' href="#" 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target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 31 - February 2, 2011 <span class="hlt">SGP</span>-TR-191 CONVERTING GEOTHERMAL PLAYS TO PROJECTS and Resources SA, Petroleum and Geothermal Group GPO Box 1671 Adelaide, South Australia, 5000, Australia e</p> <div class="credits"> <p class="dwt_author">Stanford University</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">462</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://pangea.stanford.edu/ERE/pdf/IGAstandard/SGW/2011/haeri2.pdf"> <span id="translatedtitle">PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 31 -February 2, 2011</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 31 - February 2, 2011 <span class="hlt">SGP</span>-TR-191 DISTRIBUTION OF ARSENIC IN GEOTHERMAL WATERS FROM SABALAN GEOTHERMAL FIELD, N-W IRAN Haeri A.,1 Strelbitskaya S., Porkhial S2 ., Ashayeri, A1 . 1</p> <div class="credits"> <p class="dwt_author">Stanford University</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">463</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://pangea.stanford.edu/ERE/pdf/IGAstandard/SGW/2011/mccoy.pdf"> <span id="translatedtitle">PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 31 -February 2, 2011</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 31 - February 2, 2011 <span class="hlt">SGP</span>-TR-191 GEOTHERMAL RESOURCES IN THE PACIFIC ISLANDS their untapped geothermal resources) for cost effective power production and direct-use applications. As part</p> <div class="credits"> <p class="dwt_author">Stanford University</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">464</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/servlets/purl/1009107"> <span id="translatedtitle">Southern Great Plains Newsletter</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">This months issue contains the following articles: (1) Scientists convene at <span class="hlt">SGP</span> site for complex convective cloud experiment; (2) VORTEX2 spins down; (3) Sunphotometer supports SPARTICUS (a Sun and Aureole Measurement imaging sunphotometer) campaign and satellite validation studies; and (4) Ceilometer represents first deployment of new ground-based instruments from Recovery Act.</p> <div class="credits"> <p class="dwt_author">J. Prell L. R. Roeder</p> <p class="dwt_publisher"></p> <p class="publishDate">2010-09-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">465</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://pangea.stanford.edu/ERE/pdf/IGAstandard/SGW/2011/boguslavsky.pdf"> <span id="translatedtitle">PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 31 -February 2, 2011</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">, Stanford, California, January 31 - February 2, 2011 <span class="hlt">SGP</span>-TR-191 DESIGNING THERMAL-PHYSICAL, POWER out at expeditious development rates and there are about a million power plants of this type-energy power plant, that supplies consumers with heat within constrained by them parameters, standard</p> <div class="credits"> <p class="dwt_author">Stanford University</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">466</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://pangea.stanford.edu/ERE/pdf/IGAstandard/SGW/2009/boyd.pdf"> <span id="translatedtitle">PROCEEDINGS, Thirty-Fourth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 9-11, 2009</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">and the near the bottom at the hot aquifer level, a convection cell is induced and the well becomes very nearly providing around 171o F over the entire well depth and obviously creating a convection cell bringing hot, Stanford, California, February 9-11, 2009 <span class="hlt">SGP</span>-TR-187 DESIGN OF A CONVECTION CELL FOR A DOWNHOLE HEAT</p> <div class="credits"> <p class="dwt_author">Stanford University</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">467</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://pangea.stanford.edu/ERE/research/geoth/publications/techreports/SGP-TR-169.pdf"> <span id="translatedtitle">Constant-Pressure Measurement of Steam-</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary"><span class="hlt">SGP</span>-TR-169 Constant-Pressure Measurement of Steam- Water Relative Permeability Peter A. O by measuring in-situ steam saturation more directly. Mobile steam mass fraction was established by separate steam and water inlets or by correlating with previous results. The measured steam-water relative</p> <div class="credits"> <p class="dwt_author">Stanford University</p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">468</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/extended_abs/kiedron1_pw.pdf"> <span id="translatedtitle">Kiedron(1)-PW</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Column Water Vapor from Diffuse Irradiance Column Water Vapor from Diffuse Irradiance P. W. Kiedron, J. L. Berndt, L. C. Harrison, J. J. Michalsky, and Q.-L. Min Atmospheric Sciences Research Center State University of New York Albany, New York Abstract A possibility of measuring water vapor column from diffuse irradiance, and thus the extension of optical retrievals to cloudy days, was investigated. The data from the Rotating Shadowband Spectroradiometer (RSS) during its winter deployment at the North Slope of Alaska (<span class="hlt">NSA</span>) site is used. The initial analysis covers 20 days in March 1999 that include clear, partly cloudy, and overcast days. During these days, water vapor column according to the <span class="hlt">NSA</span> site's Microwave Radiometer (MWR) varied between 1 and 5 mm. The diffuse irradiances in the 820 and 940-nm water vapor absorption bands are compared with </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">469</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/sites/nsa/docs/nsa_sop.pdf"> <span id="translatedtitle"> </span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary"> Issue: K Author: Mark D. Ivey Page 1 of 24 DR 6 / 30 / 2010 ES&H STANDARD OPERATING PROCEDURE (ES&H SOP) Title: ATMOSPHERIC RADIATION MEASUREMENT CLIMATE RESEARCH FACILITY/NORTH SLOPE OF ALASKA/ADJACENT ARCTIC OCEAN (ACRF/<span class="hlt">NSA</span>/AAO) PROJECT OPERATING PLAN (U) Location: North Slope of Alaska and Adjacent Arctic Ocean Owners: Mark D Ivey, Department 6383, Manager Mark D Ivey, Department 6383, ACRF/<span class="hlt">NSA</span>/AAO Site Project Manager and Site ES&H Coordinator Document Release or Change History: SP473406/Issue Release/Change No (Authorization No.) Date A DR E970005SA, Rev 0 07/14/97 B CN E970005SA, Rev 1 10/28/98 C CN E970005SA, Rev 2 03/15/00 </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">470</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf10/extended_abs/doran_jc.pdf"> <span id="translatedtitle">1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Optical Depths and Liquid Water Paths Optical Depths and Liquid Water Paths at the <span class="hlt">NSA</span> CART J. C. Doran, J. C. Barnard, and S. Zhong Pacific Northwest National Laboratory Richland, Washington C. J. Jakob European Centre for Medium-Range Weather Forecasts Reading, England Introduction As part of our efforts to characterize the cloud properties at the North Slope of Alaska (<span class="hlt">NSA</span>) Cloud and Radiation Testbed (CART), we have used microwave radiometers (MWRs) and multi-filter rotating shadowband radiometers (MFRSRs) at Barrow (a coastal site) and Atqasuk (an inland site) to measure liquid water paths (LWPs) and cloud optical depths ( ) during the period June through September 1999. In addition to developing a climatology of cloud properties at the two sites, which will require the </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">471</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/poster_abs/P00001"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Applications of the Aerosonde at <span class="hlt">NSA</span> Applications of the Aerosonde at <span class="hlt">NSA</span> Curry, J.A. and Holland, G.J., University of Colorado Eleventh Atmospheric Radiation Measurement (ARM) Science Team Meeting The first ARM Aerosonde flights at Barrow in April 1999 were not successful owing to the aircraft's inability to fly under severe icing conditions. However, we were sufficiently encouraged by these initial flights to pursue further developments to make feasible Aerosonde flights in the Arctic. NSF has funded a major project to establish a long-term Aerosonde facility based in Barrow. Extensive research is underway on the topic of icing mitigation. A limited but successful mission was undertaken in Barrow during August 2000. In the coming year, flights are planned for April, August 2001. We hope to be able to fly the originally proposed </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">472</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf09/extended_abs/storvold_r.pdf"> <span id="translatedtitle">storvold-99.PDF</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">ARM Participation in SHEBA: A Mini-CART Site Operated ARM Participation in SHEBA: A Mini-CART Site Operated in the Arctic Ocean from October 1997 Until October 1998 R. Storvold, J. Delamere, H. A. Eide, H. Lindquist, P. Utley, and K. Stamnes Geophysical Institute, University of Alaska Fairbanks, Alaska C. R. Turney and K. B. Widener Pacific Northwest National Laboratory Richland, Washington B. D. Zak Sandia National Laboratories Albuquerque, New Mexico Introduction The Surface Heat Budget of the Arctic Ocean (SHEBA) experiment provided a unique opportunity for the Atmospheric Radiation Measurement (ARM) Program to obtain valuable data over the Arctic Ocean by participating in SHEBA through ARM's North Slope of Alaska/Adjacent Arctic Ocean (<span class="hlt">NSA</span>/AAO) team. A mini-CART (Cloud and Radiation Testbed) site was operated by the ARM <span class="hlt">NSA</span>/AAO team at </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">473</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/meetings/2008/presentations/0310/8_Comstock_lowclouds.pdf"> <span id="translatedtitle">Cloud Properties Working Group Low Clouds Update</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Cloud Properties Working Group Cloud Properties Working Group Low Clouds Update Low Clouds Update Jennifer Comstock Jennifer Comstock Dave Turner Dave Turner Andy Andy Vogelmann Vogelmann Instruments Instruments 90/150 GHz microwave radiometer 90/150 GHz microwave radiometer Deployed during COPS AMF Deployed during COPS AMF Exploring calibration w/ DPR ( Exploring calibration w/ DPR ( Crewell Crewell & & L L ö ö hnert hnert ) ) See COPS Breakout, Wednesday evening See COPS Breakout, Wednesday evening 183 GHz (GVR) deployed at the <span class="hlt">NSA</span> 183 GHz (GVR) deployed at the <span class="hlt">NSA</span> Neural network algorithm to retrieve PWV & LWP (Maria Neural network algorithm to retrieve PWV & LWP (Maria Cadeddu Cadeddu ) ) Potential VAP candidate (RPWG) Potential VAP candidate (RPWG) </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">474</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/facility/post/15647"> <span id="translatedtitle">ARM - Facility News Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">, 2011 [Facility News] , 2011 [Facility News] Methane Monitor Joins Surface Flux Instruments at North Slope Bookmark and Share The new ECOR/SEBS Tower at the <span class="hlt">NSA</span> site in Barrow includes greenhouse gas flux instruments. At the top of the tower, left to right, are the methane sensor, sonic anemometer, and carbon dioxide and water vapor sensor. The horizontal arm below and to the left of these instruments is a net radiometer. The new ECOR/SEBS Tower at the <span class="hlt">NSA</span> site in Barrow includes greenhouse gas flux instruments. At the top of the tower, left to right, are the methane sensor, sonic anemometer, and carbon dioxide and water vapor sensor. The horizontal arm below and to the left of these instruments is a net radiometer. In October 2011, the ARM North Slope of Alaska site in Barrow welcomed a </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">475</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf15/poster_abs/P00202"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents: Establishing Continuous</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Establishing Continuous Atmospheric Profiles at the North Slope of Alaska Establishing Continuous Atmospheric Profiles at the North Slope of Alaska ACRF Delamere, Jennifer Atmospheric and Environmental Research, Inc. Turner, David Pacific Northwest National Laboratory Mlawer, Eli Atmospheric & Environmental Research, Inc. Clough, Shepard Atmospheric and Environmental Research Miller, Mark Brookhaven National Laboratory Troyan, David Brookhaven National Laboratory Clothiaux, Eugene The Pennsylvania State University Accurate and continuous vertical profiles of the atmospheric state above the North Slope of Alaska ARM Climate Research Facility (<span class="hlt">NSA</span> ACRF) are a necessity for both accurate forward radiative transfer calculations and cloud microphysical retrievals. In particular, such profiles are a critical component of two important initiatives at the <span class="hlt">NSA</span> site, the Broadband </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">476</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf08/extended_abs/zak_bd.pdf"> <span id="translatedtitle">zak-98.pdf</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">1 1 The North Slope of Alaska and Adjacent Arctic Ocean (<span class="hlt">NSA</span>/AAO) Cart Site Begins Operation: Collaboration with SHEBA and FIRE B. D. Zak, H. Church, M. Ivey, L. Yellowhorse, and J. Zirzow Sandia National Laboratories Albuquerque, New Mexico K. B. Widener, P. Rhodes, C. Turney, and A. Koontz Pacific Northwest National Laboratory Richland, Washington K. Stamnes, R. Storvold, H. A. Eide, and P. Utley Geophysical Institute University of Alaska Fairbanks, Alaska R. Eagan, D. Cook, D. Hart, and M. Wesely Argonne National Laboratory Argonne, Illinois Introduction Since the 1997 Atmospheric Radiation Measurement (ARM) Science Team Meeting, the North Slope of Alaska and Adjacent Arctic Ocean (<span class="hlt">NSA</span>/AAO) Cloud and Radiation Testbed (CART) site has come into being. Much has happened even since the 1998 Science Team </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">477</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00154.pdf"> <span id="translatedtitle">Slide 1</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Performance of Forecasting Models Across the North Slope of Alaska Performance of Forecasting Models Across the North Slope of Alaska During the Mixed-Phase Arctic Cloud Experiment Victor Yannuzzi, Eugene Clothiaux, Johannes Verlinde and Jerry Harrington The Pennsylvania State University Introduction The Mixed-Phase Arctic Cloud Experiment (MPACE) was conducted across the North Slope of Alaska (<span class="hlt">NSA</span>) from September 27 through October 22, 2004. The experiment was funded by the Department of Energy (DOE)-Atmospheric Radiation Measurement (ARM) program to study the microphysics, radiative properties, thermodynamics, and life cycle of mixed-phase clouds in the Arctic. A focused set of observation stations and soundings were in place across the <span class="hlt">NSA</span> (figure 1) where conditions could be expected to produce low-level mixed-phase clouds on </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">478</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf14/poster_abs/P00057"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Simplifying Access to the North Slope of Alaska Data Streams Simplifying Access to the North Slope of Alaska Data Streams Bahrmann, C.P.(a), Richardson, S.R.(a), Clothiaux, E.E.(a), Verlinde, J.(a), McCord, R.A.(b), and Horwedel, B.(b), Department of Meteorology, The Pennsylvania State University (a), Oak Ridge National Laboratory (b) In August 2003, the <span class="hlt">NSA</span> Site Scientist Team initiated a meta-data investigation on all <span class="hlt">NSA</span> data streams. This investigation started by examining data streams for measurement name discrepancies. For example, the nsaskyrad60sC1.a1 data stream contains the measurement from a Shaded PSP. From 1998-02-14 through 2001-03-31 the measurement was called psps_mean (PSP shaded mean). On 2003-04-01 the measurement was renamed to down_short_diffuse_hemisp (Downwelling Shortwave Diffuse Hemispheric </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">479</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/instruments/mettwr"> <span id="translatedtitle">ARM - Instrument - mettwr</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">govInstrumentsmettwr govInstrumentsmettwr Documentation METTWR : Handbook METTWR : Instrument Mentor Monthly Summary (IMMS) reports METTWR : Data Quality Assessment (DQA) reports ARM Data Discovery Browse Data Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Instrument : Surface and Tower Meteorological Instrumentation at <span class="hlt">NSA</span> (METTWR) Instrument Categories Surface Meteorology Picture of the Surface meteorological measurements from tower (METTWR) Picture of the Surface meteorological measurements from tower (METTWR) General Overview Surface and Tower Meteorological Instrumentation at <span class="hlt">NSA</span> (METTWR) use mainly conventional in situ sensors to measure wind speed, wind direction, air temperature, dew point, and humidity mounted on either a 10-m or a 40-m </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">480</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/sites/nsa/docs/nsa_cwh.pdf"> <span id="translatedtitle">Cold Weather Hazards</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">0 0 Cold Weather Hazards June 2010 <span class="hlt">NSA</span>_cwh_Rev10.doc 1 Atmospheric Radiation Measurement Climate Research Facility/ North Slope of Alaska/Adjacent Arctic Ocean (ACRF/<span class="hlt">NSA</span>/AAO) Cold Weather Hazards Winter Conditions at the North Slope of Alaska The North Slope of Alaska is north of the Arctic Circle at latitudes ranging from 69 to 72 degrees. Barrow, the largest town on the North Slope (pop. 4500), is the site of a National Weather Service Station, which has been active for several decades, so the climatology of the Alaska arctic coastal region as represented by Barrow is relatively well known. The North Slope is covered with ice and snow typically eight months of the year (October-May). During part of November, all of December, and most of January, the sun does not come above the horizon; this </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_23");' href="#" title="Previous Page"> <img id="PreviousPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.previous.18x20.png" alt="Previous Page" /></a> <span id="PageLinks" class="pageLinks"> <span> <a onClick='return showDiv("page_1");' href="#">1</a> <a 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src="http://www.osti.gov/nlesearch/images/icon.last.18x20.png" alt="Last Page" /></a> </div> <a href="http://www.osti.gov/nle/topicpages">Index</a> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">481</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf16/poster_abs/P00138"> <span id="translatedtitle">Determination of vertical profiles of aerosol extinction, single scatter</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Determination of vertical profiles of aerosol extinction, single scatter Determination of vertical profiles of aerosol extinction, single scatter albedo and asymmetry parameter at Barrow. Sivaraman, Chitra Pacific Northwest National Laboratory Flynn, Connor Pacific Northwest National Laboratory Turner, David University of Wisconsin-Madison Category: Aerosols Efforts are currently underway to run and evaluate the Broadband Heating Rate Profile project at the ARM North Slope of Alaska (<span class="hlt">NSA</span>) Barrow site for the time period March 2004 - February 2005. The Aerosol Best-Estimate (ABE) Value-Added Procedure (VAP) is to provide continuous estimates of vertical profiles of aerosol extinction, single-scatter albedo, and asymmetry parameter above the Northern Slopes of Alaska (<span class="hlt">NSA</span>) facility. In the interest of temporal continuity, we have developed an algorithm that </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">482</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/data/pi/74"> <span id="translatedtitle">ARM - PI Product - Cloud-Scale Vertical Velocity and Turbulent Dissipation</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">ProductsCloud-Scale Vertical Velocity and Turbulent ProductsCloud-Scale Vertical Velocity and Turbulent Dissipation Rate Retrievals Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send PI Product : Cloud-Scale Vertical Velocity and Turbulent Dissipation Rate Retrievals Site(s) <span class="hlt">NSA</span> General Description Time-height fields of retrieved in-cloud vertical wind velocity and turbulent dissipation rate, both retrieved primarily from vertically-pointing, Ka-band cloud radar measurements. Files are available for manually-selected, stratiform, mixed-phase cloud cases observed at the North Slope of Alaska (<span class="hlt">NSA</span>) site during periods covering the Mixed-Phase Arctic Cloud Experiment (MPACE, late September through early November 2004) and the Indirect and Semi-Direct Aerosol Campaign (ISDAC, April-early May </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">483</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/science/meetings/2006/posters/06awards/shupe.pdf"> <span id="translatedtitle">Microsoft PowerPoint - ARMST2006_mp.ppt</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Characterization of Arctic Characterization of Arctic Mixed-Phase Clouds Matthew D. Shupe a , Pavlos Kollias b , Ed Luke b a Cooperative Institute for Research in Environmental Sciences - University of Colorado and NOAA/ESRL/PSD and b Brookhaven National Laboratory, Atmospheric Science Division, Upton, NY Mixed-Phase Cloud Properties Cloud Occurrence. Mixed-phase clouds occur 45% +/- 10% of the time per year at the <span class="hlt">NSA</span> site. There is a marked increase in mixed-phase cloudiness in the spring and fall transition seasons, mostly at heights below about 1 km. All mixed-phase cloud properties presented in this panel were derived from MMCR and MWR measurements at the <span class="hlt">NSA</span> site for the time period of March 1998 through December 2004. The statistics in all plots cover this full time period. Microphysical </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">484</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf06/extended_abs/leontieva_e.pdf"> <span id="translatedtitle">Section 36</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Operation of Atmospheric Radiation Measurement Operation of Atmospheric Radiation Measurement Radiation Instruments in Fairbanks to Evaluate Performance in a Cold Environment E. Leontieva, K. Stamnes, A. Alkezweeny Geophysical Institute University of Alaska Fairbanks, Alaska B.D. Zak Sandia National Laboratories Albuquerque, New Mexico Introduction The North Slope of Alaska (<span class="hlt">NSA</span>) is an area with an adverse and severe climatological environment. Harsh weather conditions in the Arctic offer unique challenges for data collection. ifficulties associated with working in a remote locale will further complicate taking the standard radiation measurements at the <span class="hlt">NSA</span>/AAO Cloud and Radiation Testbed (CART) site. Equipment must survive low temperatures and extended periods during which maintenance will be difficult. Since the temperature in </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">485</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/poster_abs/P00051"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Differences in Cloud Characteristics at Barrow and Atqasuk at the <span class="hlt">NSA</span>/AAO Differences in Cloud Characteristics at Barrow and Atqasuk at the <span class="hlt">NSA</span>/AAO CART Doran, J.C., Barnard, J.C., Zhong, S., and Jakob, C., Pacific Northwest National Laboratory Pacific Northwest National Laboratory, European Centre for Medium-Range Weather Forecasting Eleventh Atmospheric Radiation Measurement (ARM) Science Team Meeting Data obtained from multifilter rotating shadowband radiometers (MFRSRs) and microwave radiometers (MWRs) have been used to examine the differences in the cloud characteristics at Barrow and Atqasuk during the period June-September of 1999. Because the size of a grid cell in a GCM may be on the order of 100 km or more, it is important to determine to what extent meteorological and radiometric observations made at Barrow or Atqasuk </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">486</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://energy.gov/sites/prod/files/NNSA_PO_NEPA-APS-2013.pdf"> <span id="translatedtitle">U.S. Deparment of Energy NNSA Production Ofice</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://energy.gov/">Energy.gov (U.S. Department of Energy (DOE)) Indexed Site</a></p> <p class="result-summary">Deparment of Energy Deparment of Energy NNSA Production Ofice Post Ofice Box 2050 Oak Ridge, Tennessee 37831-8009 JAN 3 1 2013 MEMORANDUM FOR GRGORY H. WOODS �"'= lC= GENERALCOUNSEL Ef= f= FROM: STEVEN C. ERHART g= N=�= |= � L= MANAGER �·= �=?= K= t : f'-J SUBJECT: <span class="hlt">NSA</span> PRODUCTION OFFICE J Reminder Regarding Annual National Environmental Policy Act Planning Summaries Please reference the memorandum from Gregory H. Woods, General Counsel, dated </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">487</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/323733"> <span id="translatedtitle">Review of science issues, deployment strategy, and status for the ARM north slope of Alaska-Adjacent Arctic Ocean climate research site</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">Recent climate modeling results point to the Arctic as a region that is particularly sensitive to global climate change. The Arctic warming predicted by the models to result from the expected doubling of atmospheric carbon dioxide is two to three times the predicted mean global warming, and considerably greater than the warming predicted for the Antarctic. The North Slope of Alaska-Adjacent Arctic Ocean (<span class="hlt">NSA</span>-AAO) Cloud and Radiation Testbed (CART) site of the Atmospheric Radiation Measurement (ARM) Program is designed to collect data on temperature-ice-albedo and water vapor-cloud-radiation feedbacks, which are believed to be important to the predicted enhanced warming in the Arctic. The most important scientific issues of Arctic, as well as global, significance to be addressed at the <span class="hlt">NSA</span>-AAO CART site are discussed, and a brief overview of the current approach toward, and status of, site development is provided. ARM radiometric and remote sensing instrumentation is already deployed and taking data in the perennial Arctic ice pack as part of the SHEBA (Surface Heat Budget of the Arctic ocean) experiment. In parallel with ARM`s participation in SHEBA, the <span class="hlt">NSA</span>-AAO facility near Barrow was formally dedicated on 1 July 1997 and began routine data collection early in 1998. This schedule permits the US Department of Energy`s ARM Program, NASA`s Arctic Cloud program, and the SHEBA program (funded primarily by the National Science Foundation and the Office of Naval Research) to be mutually supportive. In addition, location of the <span class="hlt">NSA</span>-AAO Barrow facility on National Oceanic and Atmospheric Administration land immediately adjacent to its Climate Monitoring and Diagnostic Laboratory Barrow Observatory includes NOAA in this major interagency Arctic collaboration.</p> <div class="credits"> <p class="dwt_author">Stamnes, K. [Univ. of Alaska, Fairbanks, AK (United States). Geophysical Inst.; Ellingson, R.G. [Univ. of Maryland, College Park, MD (United States). Dept. of Meteorology; Curry, J.A. [Univ. of Colorado, Boulder, CO (United States). Dept. of Aerospace and Engineering Sciences; Walsh, J.E. [Univ. of Illinois, Urbana, IL (United States). Dept. of Atmospheric Sciences; Zak, B.D. [Sandia National Labs., Albuquerque, NM (United States)</p> <p class="dwt_publisher"></p> <p class="publishDate">1999-01-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">488</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/4439823"> <span id="translatedtitle">Rocket-borne, low gravity cryogenic heat transfer experiment</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">From AIAA/<span class="hlt">NSA</span>/ASTM/IES 7th space simulation conference; Los Angeles, Calif11nia, USA (12 Nov 1973). In order to obtain steady state data on nucleate boiling heat transfer to liquid helium in a nearly zero gravity environment a rocket-borne experiment was designed, built and successfully flown. A description of the apparatus and flight is presented along with preliminary results. (auth)</p> <div class="credits"> <p class="dwt_author">Williamson, K.D. Jr.; Edeskuty, F.J.; Taylor, J.F.</p> <p class="dwt_publisher"></p> <p class="publishDate">1974-04-30T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">489</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://escholarship.org/uc/item/93n54627?query=ANP"> <span id="translatedtitle">A Briv un An Entfer (A Letter and a Reply)</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/eprints/">E-Print Network (OSTI)</a></p> <p class="result-summary">TTypwip-Tagnya** x _ r x rp^anp px p s ^ n x a*a i n ^n'a a$isnr a&n px 3 D # T O * I s p*anp n P X " nxirr o m i a^ap^as;' "a T 8 * <span class="hlt">nsa</span>^n px ? p*anp yas^aTO sfry-Tnt * Y I w x</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate">1979-01-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">490</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.osti.gov/scitech/biblio/4354779"> <span id="translatedtitle">Liquid metal fast breeder reactors, 1972--1973</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p class="result-summary">Reference to 1467 publications on liquid sodium fast breeder reactors cited in Nuclear Science Abstracts Volume 26 (1972) through Volume 27 (1973 through June) are contained in this citation to provide information on the contents of the document. References are arranged in order by the original <span class="hlt">NSA</span> abstract number which approximately places them in chronological order. Sequence numbers appear beside each reference, and the personal author index refers to these sequence numbers. The subject index refers to the original abstract numbers. (auth)</p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate">1974-01-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">491</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://dl.acm.org/citation.cfm?id=1365739.1365759&coll=DL&dl=GUIDE&CFID=253050021&CFTOKEN=99571923"> <span id="translatedtitle">A novel tele-working platform supporting public administrational bureaus</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/scienceconferences/">Science Conference Proceedings (OSTI)</a></p> <p class="result-summary">A novel Tele-Working Platform is presented, the basis of a ready-to-be-applied multi-level Tele-Working Service supporting electronic commerce and other value-added applications business plans. Being the outcome of a large-scale common project, this ... Keywords: ATM: asynchronous transfer mode, B2B: business to business, DBMS: data base management system, DCS: distributed computing system, DSL: digital subscriber line, ISDN: integrated services digital network, ORB: object request broker, PAB: public administrational bureau, <span class="hlt">TWP</span>: tele-working platform, TWPL: tele-working layer, TWS: tele-working service</p> <div class="credits"> <p class="dwt_author">P. Sotiriades; G.-P. K. Economou; K. G. Dimopoulos; D. K. Lymberopoulos</p> <p class="dwt_publisher"></p> <p class="publishDate">2006-02-01T23:59:59.000Z</p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">492</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf15/poster_abs/P00238"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents: Assessing physical</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Assessing physical processes in the ECMWF model forecasts through the ARM Assessing physical processes in the ECMWF model forecasts through the ARM <span class="hlt">SGP</span> site measurements Neggers, Roel European Centre for Medium-range Weather Forecasts (ECMWF) Cheinet, Sylvain ECMWF (UK) Beljaars, Anton ECMWF Koehler, M European Centre for Medium-range Weather Forecasts, Reading, Morcrette, Jean-Jacques European Centre for Medium-Range Weather Forecasts Viterbo, Pedro ECMWF In this study, we compare short-term weather forecasts of the ECMWF model (Integrated Forecast System, IFS) to measurements at the Southern Great Plains (<span class="hlt">SGP</span>) site of the Atmospheric Radiation Measurement (ARM) program in July 2003. By using a number of ARM instruments and complementary satellite and radar network data, a number of systematic deficiencies are characterized in the IFS, focusing on mixing processes. </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">493</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/news/features/post/17768"> <span id="translatedtitle">ARM - Feature Stories and Releases Article</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">7, 2012 [Feature Stories and Releases] 7, 2012 [Feature Stories and Releases] Southern Great Plains Site in Path of Tornado Bookmark and Share Property of several <span class="hlt">SGP</span> site personnel took a hit during the April 30 tornado. Site operations manager John Schatz shared this photo of damage to and around his barn. Property of several <span class="hlt">SGP</span> site personnel took a hit during the April 30 tornado. Site operations manager John Schatz shared this photo of damage to and around his barn. On April 30, at about 10:30 p.m, a tornado touched down in Medford, Oklahoma, northwest of the Central Facility at ARM's Southern Great Plains site. The storm track moved southeast, passing through several counties and leaving a path of destruction in its wake. In spite of winds in excess of 80 mph and baseball-sized hail, ARM instruments and structures </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">494</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf11/poster_abs/P00128"> <span id="translatedtitle">ARM - Publications: Science Team Meeting Documents</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Raman Lidar Characterization of the Vertical Variability of Aerosols and Raman Lidar Characterization of the Vertical Variability of Aerosols and Water Vapor Over the <span class="hlt">SGP</span> Ferrare, R.A. (a), Turner, D.D. (b,g), Brasseur, L.H. (c), Tooman, T.P. (d), Dubovik, O. (e), Goldsmith, J.E.M. (d), Ogren, J.A. (f), and Feltz, W. (g), NASA Langley Research Center (a), Pacific Northwest National Laboratory (b), Science Applications International Corporation/NASA/LaRC (c), Sandia National Laboratories (d), SSAI/NASA Goddard Space Flight Center (e), NOAA Climate Monitoring and Diagnostics Laboratory (f), University of Wisconsin-Madison (g) Eleventh Atmospheric Radiation Measurement (ARM) Science Team Meeting The automated Southern Great Plains (<span class="hlt">SGP</span>) Cloud and Radiation Testbed (CART) Raman Lidar routinely measures profiles of water vapor mixing ratio, </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">495</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00093.pdf"> <span id="translatedtitle">Robert Pincus and Crispian Batstone, CIRES/Univ. Colorado and NOAA Earth System Research Lab</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Characteristic atmospheric profiles at the <span class="hlt">SGP</span> site: Characteristic atmospheric profiles at the <span class="hlt">SGP</span> site: Results from the ARM continuous forcing and two climate models Robert Pincus and Crispian Batstone, CIRES/Univ. Colorado and NOAA Earth System Research Lab Amy Braverman, Jet Propulsion Laboratory Errors in climate model predictions of cloud properties stem from some combination of (at least) two causes: * the cloud parameterization may produce the wrong cloud properties from a correct atmospheric state (or history of states), or * the cloud parameterization may be driven by incorrect states. Errors seen in long-term climatologies can't distinguish between these two error sources, but the different modes of failure have very different implica- tions for model development. There are two approaches to disentangling these error sources: </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">496</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf17/poster/P00049.pdf"> <span id="translatedtitle">Microsoft PowerPoint - ARM07_3sm.ppt [Compatibility Mode]</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">Albedo Temporal and Spatial Validation at the <span class="hlt">SGP</span> Site Albedo Temporal and Spatial Validation at the <span class="hlt">SGP</span> Site Crystal Schaaf, Jicheng Liu, Miguel Román, and Alan Strahler Department of Geography and Center for Remote Sensing, Boston University, Boston, MA 02215 The newly reprocessed (Version 005) MODIS BRDF/Albedo product is now being produced from Aqua and Terra data every eight days at an increased 500-meter spatial resolution. Once reprocessing is complete, the data record will stretch from 2000 to present The spectral Analyses and intercomparisons of MODIS V005 blue-sky albedos using 8-day and 500m resolution over two ARM Southern Great Plains sites demonstrate product consistency over a broad range of spatial, temporal, and angular scales. 1km N will stretch from 2000 to present. The spectral product provides semi-empirical, kernel-driven </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">497</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf05/extended_abs/coulter2_rl.pdf"> <span id="translatedtitle">X:\ARM_19~1\PGS53-62.WPD</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">z z i , z i , z i V s , V t Session Papers 59 Figure 1. Temporal and spatial standard deviation of sensible heat flux over the <span class="hlt">SGP</span> CART site. Values are normalized by the mean sensible heat flux, as defined in the text. Using Remotely Sensed Planetary Boundary Layer Variables as Estimates of Areally Averaged Heat Flux R. L. Coulter, T. J. Martin, and D. J. Holdridge Argonne National Laboratory Argonne, Illinois Introduction Homogeneity across the Southern Great Plains (<span class="hlt">SGP</span>) Cloud and Radiation Testbed (CART) site is an issue of importance to all facets of the Atmospheric Radiation Measurement (ARM) Program. The degree to which measurements at the central facility can be used to verify, improve, or develop relationships in radiative flux models that are subsequently used in global circulation models, for </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">498</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/campaigns/aaf2006aircarb"> <span id="translatedtitle">ARM - Field Campaign - Aircraft Carbon</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">govCampaignsAircraft Carbon govCampaignsAircraft Carbon Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Campaign : Aircraft Carbon 2006.07.01 - 2008.09.30 Lead Scientist : Margaret Torn For data sets, see below. Description Airborne trace-gas measurements at ARM-<span class="hlt">SGP</span> provided valuable data for addressing carbon-cycle questions highlighted by the US Climate Change Research Program and the North American Carbon Program. A set of carbon-cycle instruments and sample collection systems were added to an ARM-managed aircraft at ARM-<span class="hlt">SGP</span> user facility. A separate (in-place) grant covered the cost of developing the instrument systems, analyzing the data, and ingesting all data to the ARM data archives. In the short-term (~1 y) we had two priorities. The first was to acquire </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result odd" lang="en"> <div class="resultNumber element">499</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/publications/proceedings/conf14/extended_abs/widener2-kb.pdf"> <span id="translatedtitle">W-Band ARM Cloud Radar - Specifications and Design</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">W-Band ARM Cloud Radar - Specifications and Design W-Band ARM Cloud Radar - Specifications and Design K. B. Widener Pacific Northwest National Laboratory Richland, Washington J. B. Mead ProSensing, Inc. Amherst, Massachusetts Abstract The Atmospheric Radiation Measurement (ARM) Program and ProSensing, Inc. have teamed to develop and deploy the W-band ARM Cloud Radar (WACR) at the <span class="hlt">SGP</span> central facility. The WACR will be co- located with the ARM millimeter wave cloud radar (MMCR) with planned operation to begin in early 2005. This radar will complement the measurements of the MMCR and will aid in filtering out insect contamination in the data. In this poster we present the design goals, expected performance characteristics, and the detailed design for the WACR. Introduction The MMCR has been operating at the Southern Great Plains (<span class="hlt">SGP</span>) site since 1998. It has proven to be </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div class="floatContainer result " lang="en"> <div class="resultNumber element">500</div> <div class="resultBody element"> <p class="result-title"><a target="resultTitleLink" href="http://www.osti.gov/nlesearch/link.html?type=RESULT&redirectUrl=http://www.arm.gov/campaigns/sgp2008assist"> <span id="translatedtitle">ARM - Field Campaign - ASSIST: Atmospheric Sounder Spectrometer for</span></a>  </p> <div class="result-meta"> <p class="source"><a target="_blank" id="logoLink" href="http://www.osti.gov/nle/index.html">NLE Websites -- All DOE Office Websites (Extended Search)</a></p> <p class="result-summary">govCampaignsASSIST: Atmospheric Sounder Spectrometer for Infrared govCampaignsASSIST: Atmospheric Sounder Spectrometer for Infrared Spectral Technology Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Campaign : ASSIST: Atmospheric Sounder Spectrometer for Infrared Spectral Technology 2008.07.08 - 2008.07.18 Lead Scientist : Michael Howard For data sets, see below. Description Goals of assist were to intercompare radiance spectra and profile retrievals from a new AERI-like instrument, called "ASSIST" with the <span class="hlt">SGP</span> site AERI(s) and calculations from Radiosondes measurements. * To bring the ASSIST instrument to the <span class="hlt">SGP</span> ACRF and perform simultaneous measurements of the sky radiation with those from the AERI. * On relatively cloud-free days, release a special radiosonde at the </p> <div class="credits"> <p class="dwt_author"></p> <p class="dwt_publisher"></p> <p class="publishDate"></p> </div> </div> </div> </div> <div id="filter_results_form" class="filter_results_form floatContainer" style="visibility: visible;"> <div style="width:90%" id="PaginatedNavigation" class="paginatedNavigationElement"> <a id="FirstPageLink" onclick='return showDiv("page_1");' href="#" title="First Page"> <img id="FirstPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.first.18x20.png" alt="First Page" /></a> <a id="PreviousPageLink" onclick='return showDiv("page_24");' href="#" title="Previous Page"> <img id="PreviousPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.previous.18x20.png" alt="Previous Page" /></a> <span id="PageLinks" class="pageLinks"> <span> <a onClick='return showDiv("page_1");' href="#">1</a> <a onClick='return showDiv("page_2");' href="#">2</a> <a onClick='return showDiv("page_3");' href="#">3</a> <a onClick='return showDiv("page_4");' href="#">4</a> <a onClick='return showDiv("page_5");' href="#">5</a> <a onClick='return showDiv("page_6");' href="#">6</a> <a onClick='return showDiv("page_7");' href="#">7</a> <a onClick='return showDiv("page_8");' href="#">8</a> <a onClick='return showDiv("page_9");' href="#">9</a> <a onClick='return showDiv("page_10");' href="#">10</a> <a onClick='return showDiv("page_11");' href="#">11</a> <a onClick='return showDiv("page_12");' href="#">12</a> <a onClick='return showDiv("page_13");' href="#">13</a> <a onClick='return showDiv("page_14");' href="#">14</a> <a onClick='return showDiv("page_15");' href="#">15</a> <a onClick='return showDiv("page_16");' href="#">16</a> <a onClick='return showDiv("page_17");' href="#">17</a> <a onClick='return showDiv("page_18");' href="#">18</a> <a onClick='return showDiv("page_19");' href="#">19</a> <a onClick='return showDiv("page_20");' href="#">20</a> <a onClick='return showDiv("page_21");' href="#">21</a> <a onClick='return showDiv("page_22");' href="#">22</a> <a onClick='return showDiv("page_23");' href="#">23</a> <a onClick='return showDiv("page_24");' href="#">24</a> <a style="font-weight: bold;">25</a> </span> </span> <a id="NextPageLink" onclick='return showDiv("page_25.0");' href="#" title="Next Page"> <img id="NextPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.next.18x20.png" alt="Next Page" /></a> <a id="LastPageLink" onclick='return showDiv("page_25.0");' href="#" title="Last Page"> <img id="LastPageLinkImage" class="Icon" src="http://www.osti.gov/nlesearch/images/icon.last.18x20.png" alt="Last Page" /></a> </div> <a href="http://www.osti.gov/nle/topicpages">Index</a> </div> </div><!-- page_25 div --> <div id="footer_inner" class="osti"> <div class="osti_footer"> <img src="http://www.osti.gov/nle/images/DOE_SC31.png" alt="USDOE" width="177" height="31" usemap="#officeofscience" border="0" /> <a href="http://www.osti.gov" title="DOE / OSTI"><img src="http://www.osti.gov/nle/images/ostigov53.png" border="0"/></a> <map name="officeofscience" id="officeofscience"> <area shape="rect" coords="4,2,126,30" href="http://energy.gov/" alt="U.S. Department of Energy" /> <area shape="rect" coords="128,1,175,31" href="http://science.energy.gov/" alt="Office of Science" /> </map> <p> Some links on this page may take you to non-federal websites. 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