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1

Grenada: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

Grenada: Energy Resources Grenada: Energy Resources Jump to: navigation, search Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"TERRAIN","zoom":5,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"390px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":12.11667,"lon":-61.66667,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

2

Grenada-Caribbean Community (CARICOM) Sustainable Energy Roadmap and  

Open Energy Info (EERE)

Grenada-Caribbean Community (CARICOM) Sustainable Energy Roadmap and Grenada-Caribbean Community (CARICOM) Sustainable Energy Roadmap and Strategy Jump to: navigation, search Name Grenada-Caribbean Community (CARICOM) Sustainable Energy Roadmap and Strategy Agency/Company /Organization Inter-American Development Bank, World Watch Institute (WWI) Sector Climate, Energy Focus Area Renewable Energy, Economic Development, Energy Efficiency, Greenhouse Gas, Grid Assessment and Integration, Industry, People and Policy, Transportation Topics Background analysis, Baseline projection, Finance, GHG inventory, Implementation, Low emission development planning, -Roadmap, Market analysis, Policies/deployment programs, Resource assessment, Technology characterizations Program Start 2012 Program End 2012 Country Grenada Caribbean

3

Grenada-Regional Implementation Plan for CARICOM's Climate Change  

Open Energy Info (EERE)

Grenada-Regional Implementation Plan for CARICOM's Climate Change Grenada-Regional Implementation Plan for CARICOM's Climate Change Resilience Framework Jump to: navigation, search Name Grenada-Regional Implementation Plan for CARICOM's Climate Change Resilience Framework Agency/Company /Organization Climate and Development Knowledge Network (CDKN), United Kingdom Department for International Development, Caribbean Community Climate Change Centre (CCCCC) Partner Caribbean Community Climate Change Centre (CCCCC), Caribbean Community Heads of State (CARICOM) Sector Climate, Energy, Land Topics Adaptation, Background analysis, Low emission development planning, -LEDS, Market analysis, Pathways analysis Website http://cdkn.org/project/planni Program Start 2009 Program End 2015 Country Grenada Caribbean References CDKN-CARICOM-A Regional Implementation Plan for CARICOM's Regional Climate Change Resilience Framework[1]

4

Grenada-Pilot Program for Climate Resilience (PPCR) | Open Energy  

Open Energy Info (EERE)

Grenada-Pilot Program for Climate Resilience (PPCR) Grenada-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Grenada-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Grenada UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

5

Guadeloupe: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

Guadeloupe: Energy Resources Guadeloupe: Energy Resources Jump to: navigation, search Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"TERRAIN","zoom":5,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"390px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":16.25,"lon":-61.58333,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

6

Grenada-Caribbean Solar Finance Program | Open Energy Information  

Open Energy Info (EERE)

form form View source History View New Pages Recent Changes All Special Pages Semantic Search/Querying Get Involved Help Apps Datasets Community Login | Sign Up Search Page Edit with form History Facebook icon Twitter icon » Grenada-Caribbean Solar Finance Program Jump to: navigation, search Name Grenada-Caribbean Solar Finance Program Agency/Company /Organization Organization of American States (OAS) Focus Area Renewable Energy, Solar Topics Finance, Background analysis Resource Type Training materials Program Start 2008 Program End 2010 Country Grenada UN Region Latin America and the Caribbean References OAS Project Database[1] "The CSFP program promotes the use of Solar Hot Water Systems through: (1) a training program for lending officers, (2) a consumer awareness campaign,

7

Grenada County, Mississippi: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

Grenada County, Mississippi: Energy Resources Grenada County, Mississippi: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 33.7516314°, -89.8130356° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":33.7516314,"lon":-89.8130356,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

8

The University of Mississippi-Grenada offers graduate degree programs geared to working adults, including  

E-Print Network (OSTI)

class, textbook costs, a laptop computer, and a classroom instruc- tional enhancement grant. Further Administration) prepare professional educators to become school administra- tors.This program can be completed-Grenada ITC Building Find us on Facebook! #12;UM/ School District Bank Hours The UM School of Education offers

Tchumper, Gregory S.

9

Hydrogeological model of a high energy geothermal field (Bouillante area, Guadeloupe, French West Indies)  

E-Print Network (OSTI)

1 Hydrogeological model of a high energy geothermal field (Bouillante area, Guadeloupe, French West, France 3. BRGM, Department of Geothermal Energy 3, Av. Claude Guillemin - 45060 Orléans Cedex 2, France Abstract The Bouillante geothermal field presently provides about 8% of the annual electricity needs

Paris-Sud XI, Université de

10

A new bed elevation dataset for Greenland  

E-Print Network (OSTI)

A new bed elevation dataset for Greenland J. L. Bamber 1 ,al. : A new bed elevation dataset for Greenland Howat, I. M.al. : A new bed elevation dataset for Greenland Fig. 3. (a)

2013-01-01T23:59:59.000Z

11

From Greenland to green lakes  

Science Journals Connector (OSTI)

From Greenland to green lakes: Cultural eutrophication and the loss of benthic pathways in .... Kahlert 2001), the importance of attached algae as an energy.

2003-06-16T23:59:59.000Z

12

Origin and diagenesis of lignin and carbohydrates in mangrove sediments of Guadeloupe (French West Indies): Evidence for a  

E-Print Network (OSTI)

Origin and diagenesis of lignin and carbohydrates in mangrove sediments of Guadeloupe (French West the molecular composition (carbohydrates and lignin-derived phenols) of these organic deposits in relationship synthesized by bacteria. On the other hand, lignin phenols were lost rather slowly, i.e. at a similar or lower

Paris-Sud XI, Université de

13

Reply to comment on "Electrical Tomography of La Soufrire of Guadeloupe Volcano: Field experiments, 1D inversion and  

E-Print Network (OSTI)

Discussion Reply to comment on "Electrical Tomography of La Soufrière of Guadeloupe Volcano: Field.25.Qi; 91.35.Pn; 91.40.-k; 93.30.Vs 1. Introduction We thank Linde and Revil for their comment [1 and discuss our approach for interpreting electrical resistivity data acquired over complex geological

Beauducel, François

14

A New Greenland Deep Ice Core  

Science Journals Connector (OSTI)

...isotopic profile with that from camp Century and with a deep-sea foraminifera...deep-sea cores. The redated Camp Century record suggests a dramatic termination...CENTURIES OF CLIMATIC RECORD FROM CAMP CENTURY ON GREENLAND ICE SHEET, SCIENCE...

W. Dansgaard; H. B. Clausen; N. Gundestrup; C. U. Hammer; S. F. Johnsen; P. M. Kristinsdottir; N. Reeh

1982-12-24T23:59:59.000Z

15

Modeling convection in the Greenland Sea  

E-Print Network (OSTI)

A detailed examination of the development of a deep convection event observed in the Greenland Sea in 1988-89 is carried out through a combination of modeling, scale estimates, and data analysis. We develop a prognostic ...

Bhushan, Vikas

1998-01-01T23:59:59.000Z

16

Greenland New Energy | Open Energy Information  

Open Energy Info (EERE)

Greenland New Energy Greenland New Energy Jump to: navigation, search Name Greenland New Energy Place Zhenjiang, Jiangsu Province, China Sector Solar Product China-based firm involved in silicon thin film solar cell technology. Coordinates 31.966261°, 119.472687° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":31.966261,"lon":119.472687,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

17

ICE CORE RECORDS | Greenland Stable Isotopes  

Science Journals Connector (OSTI)

Abstract Greenland ice cores contain a wealth of information on past climatic conditions throughout the Northern Hemisphere. A historical perspective on the climatic interpretation of stable isotopes in water and ice is presented in the introduction, while the remainder of the article is devoted to the current interpretation of stable isotope data from Greenland ice cores. The progress in our understanding of stable isotope signals, on timescales from seasons to glacial cycles, is discussed and evaluated through numerous examples from Greenland ice cores. Stable isotope profiles from the Camp Century, Dye-3, GISP2, GRIP, NGRIP, and Renland deep ice cores are emphasized, as they all provide climatic information dating back into the Eemian period.

B.M. Vinther; S.J. Johnsen

2013-01-01T23:59:59.000Z

18

One Thousand Centuries of Climatic Record from Camp Century on the Greenland Ice Sheet  

Science Journals Connector (OSTI)

...Centuries of Climatic Record from Camp Century on the Greenland Ice Sheet 10...depth has been evaluated for the Camp Century, Greenland, 1390 meter deep ice...THEORETICAL TEMPERATURE PROFILES OF CAMP CENTURY GREENLAND BOREHOLE, JOURNAL OF...

W. Dansgaard; S. J. Johnsen; J. Mller; C. C. Langway Jr.

1969-10-17T23:59:59.000Z

19

ARM - Field Campaign - Lidar support for ICECAPS at Summit, Greenland  

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

govCampaignsLidar support for ICECAPS at Summit, Greenland govCampaignsLidar support for ICECAPS at Summit, Greenland Campaign Links ICECAPS Campaign Summary (PDF) Summit Station Research Highlight New Data from Greenland for Arctic Climate Research Cloud Cocktail Melts Greenland Ice Sheet Comments? We would love to hear from you! Send us a note below or call us at 1-888-ARM-DATA. Send Campaign : Lidar support for ICECAPS at Summit, Greenland 2010.04.15 - 2014.10.31 Lead Scientist : David Turner Description Beginning in May 2010, the Integrated Characterization of Energy, Clouds, Atmospheric State, and Precipitation over Summit (ICECAPS) project, funded through the National Science Foundation's Arctic Observing Network, is deploying a suite of remote sensors at Summit, Greenland, for four years. With dining facilities and communications gear, the "Big House" at Summit Station serves as the central gathering area for site researchers. (Photo courtesy Summit Station.)

20

Methanesulfonate in the Greenland Ice Sheet Project 2 Ice Core  

E-Print Network (OSTI)

sulfate in the Dye 3 and Camp Century Greenland ice cores infor SO4 2- in the Dye 3, Camp Century, MSA to non-sea salt

Saltzman, E. S; Whung, P.-Y.; Mayewski, P. A

1997-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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

Team advances understanding of the Greenland Ice Sheet's meltwater...  

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

for Greenland in the future, but its impact on ice sheet flux and associated sea level rise is uncertain: direct observations of the subglacial drainage system are lacking...

22

The Risk Assessment Information System  

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

RAIS User's Group RAIS User's Group The connection is no longer here Fill out the following section for addition to the RAIS User's List: CONTACT DETAILS First name: * Required Last name: * Required Company: Street: City: State: Country: Anguilla Antigua and Barbuda Aruba Bahamas Barbados Belize Bermuda Virgin Islands, British Canada Cayman Islands Costa Rica Cuba Dominica Dominican Republic El Salvador Falkland Islands (Malvinas) Greenland Grenada Guadeloupe Guatemala Haiti Honduras Jamaica Martinique Mexico Montserrat Netherlands Antilles Nicaragua Panama Puerto Rico Saint Kitts and Nevis Saint Lucia Saint Pierre and Miquelon Saint Vincent and The Grenadines Trinidad and Tobago Turks and Caicos Islands United States United States Minor Outlying Islands Virgin Islands, U.S. Argentina Bolivia

23

Extensional evolution of the central East Greenland Caledonides  

E-Print Network (OSTI)

This thesis addresses the complexity of both syn- and post-orogenic extension in the overriding plate during Caledonian continental collision through field and laboratory investigations in the central East Greenland ...

White, Arthur Percy, 1972-

2001-01-01T23:59:59.000Z

24

Meltwater effects on flow of Greenland's ice sheet less severe...  

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

severe than feared Meltwater effects on flow of Greenland's ice sheet less severe for sea level rise than earlier feared, scientists say The team found that accelerating ice sheet...

25

Greenland: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

Page Page Edit with form History Facebook icon Twitter icon » Greenland: Energy Resources Jump to: navigation, search Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"TERRAIN","zoom":5,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"390px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":72,"lon":-40,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

26

Multi-Annual Changes in Microwave Backscatter over the Greenland Ice Sheet  

E-Print Network (OSTI)

Multi-Annual Changes in Microwave Backscatter over the Greenland Ice Sheet Ivan S. Ashcraft in the location of key ice facies/zones on the Greenland ice sheet are considered key indicators of global climate the SIR al- gorithm to produce u" images, the meiisurements made by these sensors over Greenland

Long, David G.

27

Ice Core Evidence for Extensive Melting of the Greenland Ice Sheet in the Last Interglacial  

Science Journals Connector (OSTI)

...the Canadian Arctic Islands and Camp Century and Dye-3 in Greenland suggests...the Canadian Arctic Islands and Camp Century and Dye-3 in Greenland suggests...the Canadian Arctic Islands and Camp Century and Dye-3 in Greenland suggests...

R. M. Koerner

1989-05-26T23:59:59.000Z

28

Be dating of the Narsarsuaq moraine in southernmost Greenland: evidence for a late-Holocene ice advance exceeding the Little Ice Age  

E-Print Network (OSTI)

in southern Greenland. Southern Greenland warming at w1.5 ka was also concurrent with the end of the Roman Greenland. Other southernmost Greenland ice-margin records do not preclude a pre-LIA ice-margin maximum a late-Holocene pre-LIA maximum was a local phe- nomenon or a regional southern Greenland ice maximum

29

Aluminum-26 and Beryllium-10 in Greenland Ice  

Science Journals Connector (OSTI)

...100-to 300-year-old ice at Camp Century, Greenland, have been described...liter. The precipitation rate at Camp Century is well known from stratigraphic...precipitation in particulate material at Camp Century now stands at 0.6 X 10-8 dpm...

R. McCorkell; E. L. Fireman; C. C. Langway Jr.

1967-12-29T23:59:59.000Z

30

The first Greenland ice core record of methanesulfonate and sulfate over a full glacial cycle  

E-Print Network (OSTI)

sulf,te in the Dye 3 and Camp Century, Greenland ice cores,in both the Dye 3 and Camp Century deep ice cores [Herron

Hansson, Margareta E; Saltzman, Eric S

1993-01-01T23:59:59.000Z

31

Greenland, New Hampshire: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

Greenland, New Hampshire: Energy Resources Greenland, New Hampshire: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 43.0361995°, -70.8328322° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":43.0361995,"lon":-70.8328322,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

32

The Greenland Telescope (GLT): Antenna status and future plans  

E-Print Network (OSTI)

The ALMA North America Prototype Antenna was awarded to the Smithsonian Astrophysical Observatory (SAO) in 2011. SAO and the Academia Sinica Institute of Astronomy & Astrophysics (ASIAA), SAO's main partner for this project, are working jointly to relocate the antenna to Greenland to carry out millimeter and submillimeter VLBI observations. This paper presents the work carried out on upgrading the antenna to enable operation in the Arctic climate by the GLT Team to make this challenging project possible, with an emphasis on the unexpected telescope components that had to be either redesigned or changed. Five-years of inactivity, with the antenna laying idle in the desert of New Mexico, coupled with the extreme weather conditions of the selected site in Greenland have it necessary to significantly refurbish the antenna. We found that many components did need to be replaced, such as the antenna support cone, the azimuth bearing, the carbon fiber quadrupod, the hexapod, the HVAC, the tiltmeters, the antenna ...

Raffin, Philippe; Asada, Keichi; Blundell, Raymond; Burgos, Roberto; Chang, Chih-Cheng; Chen, Ming-Tang; Christensen, Robert; Grimes, Paul K; Han, C C; Ho, Paul T P; Huang, Yau-De; Inoue, Makoto; Koch, Patrick M; Kubo, Derek; Leiker, Steve; Liu, Ching-Tang; Martin-Cocher, Pierre; Matsushita, Satoki; Nakamura, Masanori; Nishioka, Hiroaki; Nystrom, George; Paine, Scott N; Patel, Nimesh A; Pradel, Nicolas; Pu, Hung-Yi; Shen, H -Y; Snow, William; Sridharan, T K; Srinivasan, Ranjani; Tong, Edward; Wang, Jackie

2014-01-01T23:59:59.000Z

33

Observed runoff, jokulhlaups and suspended sediment load from the Greenland ice at Kangerlussuaq, West Greenland, 2007 and 2008  

SciTech Connect

This study fills the gap in hydrologic measurements of runoff exiting a part of the Greenland Ice Sheet (GrIS), the Kangerlussuaq drainage area, West Greenland. The observations are of value for obtaining knowledge about the terrestrial freshwater and sediment output from part of the GrIS and the strip of land between the GrIS and the ocean, in the context of varying ice sheet surface melt and influx entering the ocean. High-resolution stage, discharge and suspended sediment load show a decrease in runoff of {approx} 25% and in sediment load of {approx} 40% from 2007 to 2008 in response to a decrease in the summer accumulated number of positive degree days. During the 2007 and 2008 runoff season, joekulhlaups are observed at Kangerlussuaq, drained from an ice-dammed lake at the margin of the GrIS.

Mernild, Sebastian Haugard [Los Alamos National Laboratory; Hasholt, Bent [UNIV OF COPENHAGEN

2009-01-01T23:59:59.000Z

34

Response of a marineterminating Greenland outlet glacier to abrupt cooling 8200 and 9300 years ago  

E-Print Network (OSTI)

that Jakobshavn Isbræ advanced to deposit moraines in response to abrupt cooling recorded in central Greenland ice glaciers are also able to respond quickly to cooling. We suggest that short lag times of high ice fluxResponse of a marineterminating Greenland outlet glacier to abrupt cooling 8200 and 9300 years ago

Briner, Jason P.

35

Maximum late Holocene extent of the western Greenland Ice Sheet during the late 20th century  

E-Print Network (OSTI)

the 20th century. This suggests a lagged ice-margin response to prior cooling, such as the Little Ice AgeMaximum late Holocene extent of the western Greenland Ice Sheet during the late 20th century Samuel Keywords: Greenland Ice Sheet Little Ice Age 10 Be exposure dating Ice-dammed lake Lake sediment core a b

Briner, Jason P.

36

Gas isotopes in ice reveal a vegetated central Greenland during ice sheet invasion  

E-Print Network (OSTI)

= ) in the silty ice, reaching values as high as 22 mM [Tison et al., 1998]. Ammonium oxalate is produced duringGas isotopes in ice reveal a vegetated central Greenland during ice sheet invasion R. Souchez,1 J prevailing during build-up of the Greenland Ice Sheet (GIS) are not yet established. Here we use results from

Chappellaz, Jérôme

37

Greenland ice sheet surface mass balance variability (1988-2004) from calibrated Polar MM5 output*  

E-Print Network (OSTI)

1 Greenland ice sheet surface mass balance variability (1988-2004) from calibrated Polar MM5 output in Environmental Sciences, University of Colorado, Boulder, CO, USA 4 National Snow and Ice Data Center, University coherent regional patterns of Greenland ice sheet surface mass balance (SMB) change over a 17-year period

Howat, Ian M.

38

Ocean circulation and properties in Petermann Fjord, Greenland H. L. Johnson,1  

E-Print Network (OSTI)

Ocean circulation and properties in Petermann Fjord, Greenland H. L. Johnson,1 A. Münchow,2 K. K of oceanic heat entering the fjord. Citation: Johnson, H. L., A. Münchow, K. K. Falkner, and H. Melling (2011

Johnson, Helen

39

Model estimates of the mass balance of the Greenland and Antartic ice sheets  

E-Print Network (OSTI)

The six possible combinations of two climate models and three methods for calculating the melting of snow and ice are used to estimate current values of accumulation and ablation on the Greenland and Antarctic ice sheets. ...

Bugnion, Vronique.

40

Runoff simulations from the Greenland ice sheet at Kangerlussuaq from 2006-2007 to 2007/08. West Greenland  

SciTech Connect

This study focuses on runoff from a large sector of the Greenland Ice Sheet (GrIS) - the Kangerlussuaq drainage area, West Greenland - for the runoff observation period 2006/07 to 2007/08. SnowModel, a state-of-the-art snow-evolution modeling system, was used to simulate winter accumulation and summer ablation processes, including runoff. Independent in situ end-of-winter snow depth and high-resolution runoff observations were used for validation of simulated accumulation and ablation processes. Runoff was modeled on both daily and hourly time steps, filling a data gap of runoff exiting part of the GrIS. Using hourly meteorological driving data instead of smoothed daily-averaged data produced more realistic meteorological conditions in relation to snow and melt threshold surface processes, and produced 6-17% higher annual cumulative runoff. The simulated runoff series yielded useful insights into the present conditions of inter-seasonal and inter-annual variability of Kangerlussuaq runoff, and provided an acceptable degree of agreement between simulated and observed runoff. The simulated spatial runoff distributions, in some areas of the GrIS terminus, were as high as 2,750 mm w.eq. of runoff for 2006/07, while only 900 mm w.eq was simulated for 2007/08. The simulated total runoff from Kangerlussuaq was 1.9 km{sup 3} for 2006/07 and 1.2 km{sup 3} for 2007/08, indicating a reduction of 35-40% caused by the climate conditions and changes in the GrIS freshwater storage. The reduction in runoff from 2006/07 to 2007/08 occurred simultaneously with the reduction in the overall pattern of satellite-derived GrIS surface melt from 2007 to 2008.

Mernild, Sebastian Haugard [Los Alamos National Laboratory; Hasholt, Bent [UNIV OF COPENHAGEN; Van Den Broeke, Michiel [UTRECHT UNIV; Liston, Glen [COLORADO STATE UNIV

2009-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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

Complexity of Holocene Climate as Reconstructed from a Greenland Ice Core  

Science Journals Connector (OSTI)

...RESEARCH-ATMOSPHERES 91 , 1067 ( 1986 ). FISHER D.A. , C-14 PRODUCTION COMPARED TO OXYGEN ISOTOPE RECORDS FROM CAMP CENTURY, GREENLAND AND DEVON ISLAND, CANADA , CLIMATIC CHANGE 4 , 419 ( 1982 ). GROOTES P.M. , COMPARISON OF OXYGEN-ISOTOPE RECORDS...

S. R. O'Brien; P. A. Mayewski; L. D. Meeker; D. A. Meese; M. S. Twickler; S. I. Whitlow

1995-12-22T23:59:59.000Z

42

Mercury in a Greenland Ice Sheet: Evidence of Recent Input by Man  

Science Journals Connector (OSTI)

...basis of this work. The Greenland samples were from the Camp Century area (770l0'N, 61007'W) and from a virgin site...were recovered from the walls of an inclined shaft at Camp Century, and the sam-ples of more recent ages were taken...

Herbert V. Weiss; Minoru Koide; Edward D. Goldberg

1971-11-12T23:59:59.000Z

43

Selenium and Sulfur in a Greenland Ice Sheet: Relation to Fossil Fuel Combustion  

Science Journals Connector (OSTI)

...selenium content of these samples was determined by measurement of neutron induced 81Se. The samples were from the Camp Century area of the Greenland ice sheet (77 10'N and 61 07'W) and from a virgin area 80 km east southeast of this location...

Herbert V. Weiss; Minoru Koide; Edward D. Goldberg

1971-04-16T23:59:59.000Z

44

Interglacial High Sea Levels and the Control of Greenland Ice by the Precession of the Equinoxes  

Science Journals Connector (OSTI)

...ages. BROECKER, W.S., SCIENCE 151 : 299 ( 1968 ). DANSGAARD, W, ONE THOUSAND CENTURIES OF CLIMATIC RECORD FROM CAMP CENTURY ON GREENLAND ICE SHEET, SCIENCE 166 : 377 ( 1969 ). EMILIANI, C, CARIBBEAN CORES P6304-8 AND P6304-9 - NEW ANALYSIS...

C. Emiliani

1969-12-19T23:59:59.000Z

45

Challenges to Understanding the Dynamic Response of Greenland's Marine Terminating Glaciers to Oceanic and Atmospheric Forcing  

E-Print Network (OSTI)

The recent retreat and speedup of outlet glaciers, as well as enhanced surface melting around the ice sheet margin, have increased Greenland's contribution to sea level rise to 0.6 0.1 mm yr[superscript ?1] and its ...

Straneo, Fiammetta

46

Greenland temperature, climate change, and human society during the last 11,600 years  

E-Print Network (OSTI)

enabling winter sea ice cover and cooling of Greenland mean-as large as the Little Ice Age cooling (~1.6 C after theand GRIP ice cores corresponds to 2.7 C cooling, using the

Kobashi, Takuro

2007-01-01T23:59:59.000Z

47

Improving the precision of otolith-based age estimates for Greenland halibut  

E-Print Network (OSTI)

and Lyons, 1991). The latter is the primary cause of low pre- cision with Greenland halibut-4 DK-1261 Copenhagen K Denmark. 2 Alpoim, R., E. Roman, B. Greene, R. Burry, and W. R. Bowering. 2002; Kuznetsova et al., 2001; Al- poim et al.2). To date these processes have had equivocal effects on the pre

48

Abrupt climate shifts in Greenland due to displacements of the sea ice edge  

E-Print Network (OSTI)

by insulating the atmosphere from the substantial heat capacity of the ocean. When sea ice is absent, the oceanAbrupt climate shifts in Greenland due to displacements of the sea ice edge Camille Li,1 David S that a reduction in sea ice extent in the North Atlantic produces a climatic response consistent with abrupt

Schrag, Daniel

49

Improvement of radar ice-thickness measurements of Greenland outlet glaciers using SAR processing  

E-Print Network (OSTI)

Extensive aircraft-based radar ice-thickness measurements over the interior and outlet-glacier regions of the Greenland ice sheet have been obtained by the University of Kansas since 1993, with the latest airborne surveys conducted in May 2001...

Braaten, David A.; Gogineni, S. Prasad; Tammana, Dilip; Namburi, Saikiran; Paden, John; Gurumoorthy, Krishna K.

2002-01-01T23:59:59.000Z

50

Remote sensing of Greenland ice sheet using multispectral near-infrared and visible radiances  

E-Print Network (OSTI)

Remote sensing of Greenland ice sheet using multispectral near-infrared and visible radiances Petr remote-sensing algorithm that utilizes reflected visible and near-infrared radiation to discriminate using multispectral near-infrared and visible radiances, J. Geophys. Res., 112, D24S20, doi:10

Dozier, Jeff

51

Challenges to Understanding the Dynamic Response of Greenland's Marine Terminating Glaciers to Oceanic and Atmospheric Forcing  

Science Journals Connector (OSTI)

The recent retreat and speedup of outlet glaciers, as well as enhanced surface melting around the ice sheet margin, have increased Greenland's contribution to sea level rise to 0.6 0.1 mm yr?1 and its discharge of freshwater into the North Atlantic. The ...

Fiammetta Straneo; Patrick Heimbach; Olga Sergienko; Gordon Hamilton; Ginny Catania; Stephen Griffies; Robert Hallberg; Adrian Jenkins; Ian Joughin; Roman Motyka; W. Tad Pfeffer; Stephen F. Price; Eric Rignot; Ted Scambos; Martin Truffer; Andreas Vieli

2013-08-01T23:59:59.000Z

52

Dissipation Rate Estimates from Microstructure and Finescale Internal Wave Observations along the A25 GreenlandPortugal OVIDE Line  

Science Journals Connector (OSTI)

A total of 96 finestructure and 30 microstructure full-depth vertical profiles were collected along the A25 GreenlandPortugal Observatoire de la Variabilit Interannuelle et Dcennale en Atlantique Nord (OVIDE) hydrographic line in 2008. The ...

Bruno Ferron; Florian Kokoszka; Herl Mercier; Pascale Lherminier

2014-11-01T23:59:59.000Z

53

Caribbean-NREL Cooperation | Open Energy Information  

Open Energy Info (EERE)

Anguilla, Antigua and Barbuda, Aruba, Bahamas, Barbados, Cuba, Dominica, Dominican Republic, Grenada, Guadeloupe, Haiti, Jamaica, Martinique, Saint Kitts and Nevis, Saint Lucia, Saint Vincent and the Grenadines, Trinidad and Tobago, Turks and Caicos Islands Anguilla, Antigua and Barbuda, Aruba, Bahamas, Barbados, Cuba, Dominica, Dominican Republic, Grenada, Guadeloupe, Haiti, Jamaica, Martinique, Saint Kitts and Nevis, Saint Lucia, Saint Vincent and the Grenadines, Trinidad and Tobago, Turks and Caicos Islands UN Region Latin America and the Caribbean References NREL International Program [1] Abstract The National Renewable Energy Laboratory is partnering with Caribbean nations to build Low Carbon Communities in the Caribbean as part of the broader Low Carbon Communities of the Americas program.... The National Renewable Energy Laboratory is partnering with Caribbean nations to build Low Carbon Communities in the Caribbean as part of the broader Low Carbon Communities of the Americas program. References

54

Tracer transport in the Greenland Ice Sheet: constraints on ice cores and glacial history  

Science Journals Connector (OSTI)

The climate history and dynamics of the Greenland Ice Sheet are studied using a coupled model of the depositional provenance and transport of glacier ice, allowing simultaneous prediction of the detailed isotopic stratigraphy of ice cores at all the major Greenland sites. Adopting a novel method for reconstructing the agedepth relationship, we greatly improve the accuracy of semi-Lagrangian tracer tracking schemes and can readily incorporate an age-dependent ice rheology. The larger aim of our study is to impose new constraints on the glacial history of the Greenland Ice Sheet. Leading sources of uncertainty in the climate and dynamic history are encapsulated in a small number of parameters: the temperature and elevation isotopic sensitivities, the glacialinterglacial precipitation contrast and the effective viscosity of ice in the flow law. Comparing predicted and observed ice layering at ice core sites, we establish plausible ranges for the key model parameters, identify climate and dynamic histories that are mutually consistent and recover the past depositional elevation of ice cores to ease interpretation of their climatic records. With the coupled three-dimensional model of ice dynamics and provenance transport we propose a method to place all the ice core records on a common time scale and use discrepancies to adjust the reconstructed climate history. Analysis of simulated GRIP ice layering and borehole temperature profiles confirms that the GRIP record is sensitive to the dynamic as well as to the climatic history, but not enough to strongly limit speculation on the state of the Greenland Ice Sheet during the Eemian. In contrast, our study indicates that the Dye 3 and Camp Century ice cores are extremely sensitive to ice dynamics and greatly constrain Eemian ice sheet reconstructions. We suggest that the maximum Eemian sea-level contribution of the ice sheet was in the range of 3.54.5m.

Nicolas Lhomme; Garry K.C. Clarke; Shawn J. Marshall

2005-01-01T23:59:59.000Z

55

Be climate fingerprints during the Eemian in the NEEM ice core, Greenland  

E-Print Network (OSTI)

as well as the ice chronology. 10 Be (half-life 5 1.387 6 0.012 3 106 years3 ;) is mainly produced10 Be climate fingerprints during the Eemian in the NEEM ice core, Greenland Anna Sturevik-Storm1 of Geology, Lund University, So¨lvegatan 12, 223 62 Lund, Sweden, 5 Centre for Ice and Climate, Niels Bohr

Usoskin, Ilya G.

56

The distribution and ecology of benthic Foraminifera and associated meiofauna in the Northeast Water Polynya, Greenland  

E-Print Network (OSTI)

THE DISTRIBUTION AND ECOLOGY OF BENTHIC FORAMINIFERA AND ASSOCIATED MEIOFAUNA IN THE NORTHEAST WATER POLYNYA, GREENLAND A Thesis by ADRIAN CHARLES NEWTON Submitted to Texas ASSAM University in partial fulfillment of the requirements... for the degree of MASTER OF SCIENCE Approved as to style and content by: Gilbert T. Rowe (Chair of Committee) Niall Slowe (Member) R, 'rt . ta n (Member John atm uth (Head of Department) August 1994 Major Subject: Oceanography ABSTRACT...

Newton, Adrian Charles

2012-06-07T23:59:59.000Z

57

Total All Countries Exports of Crude Oil and Petroleum Products by  

U.S. Energy Information Administration (EIA) Indexed Site

Destination: Total All Countries Afghanistan Albania Algeria Andora Angola Anguilla Antigua and Barbuda Argentina Armenia Aruba Australia Austria Azerbaijan Bahama Islands Bahrain Barbados Belarus Belgium Belize Benin Bolivia Bosnia and Herzegovina Brazil Brunei Bulgaria Burma Bermuda Cambodia Cameroon Canada Cayman Islands Chad Chile China Colombia Congo (Brazzaville) Congo (Kinshasa) Costa Rica Croatia Cyprus Czech Republic Denmark Djbouti Dominica Dominican Republic Ecuador Egypt El Salvador Equatorial Guinea Eritrea Estonia Ethiopia Fiji Finland France French Guiana French Pacific Islands Gabon Georgia, Republic of Germany Ghana Gibraltar Greece Greenland Grenada Guadeloupe Guatemala Guinea Guyana Haiti Honduras Hong Kong Hungary Iceland India Indonesia Iran Iraq Ireland Israel Italy Ivory Coast Jamaica Japan Jordon Kazakhstan Kenya Korea, South Korea, North Kyrgyzstan Kutubu Kuwait Latvia Lebanon Liberia Libya Lithuania Macau S.A.R. Macedonia Madagascar Malaysia Maldives Mali Malta Marshall Islands Mauritania Mauritius Mexico Micronesia, Federated States of Midway Islands Moldova Monaco Mongolia Montenegro Montserrat Morocco Mozambique Namibia Nepal Netherlands Netherlands/Antilles New Caledonia New Zealand Nicaragua Niger Nigeria Niue Norway Oman Pakistan Panama Papau New Guinea Paracel Islands Paraguay Peru Philippines Poland Portugal Puerto Rico Qatar Romania Russia St. Kitts and Nevis St. Lucia St. Pierre and Miquelon St. Vincent and the Grenadines Samoa San Marino Saudi Arabia Senegal Serbia and Montenegro Seychelles Sierra Leone Singapore Slovakia Slovenia Soloman Islands South Africa Spain Spratly Islands Sri Lanka Sudan Suriname Swaziland Sweden Switzerland Syria Taiwan Tanzania Thailand Tonga Togo Trinidad and Tobago Tunisia Turkey Turkmenistan Turks and Caicos Islands Uganda Ukraine United Arab Emirates United Kingdom Uruguay Uzbekistan Vanuatu Venezuela Vietnam Virgin Islands (British) Virgin Islands (U.S.) Yemen Yugoslavia Zambia Period-Unit: Monthly-Thousand Barrels Monthly-Thousand Barrels per Day Annual-Thousand Barrels Annual-Thousand Barrels per Day

58

Total Net Imports of Crude Oil and Petroleum Products into the U.S.  

U.S. Energy Information Administration (EIA) Indexed Site

Country: Total All Countries Persian Gulf OPEC Algeria Angola Ecuador Iran Iraq Kuwait Libya Nigeria Qatar Saudi Arabia United Arab Emirates Venezuela Non OPEC Afghanistan Albania Andora Anguilla Antigua and Barbuda Argentina Armenia Aruba Australia Austria Azerbaijan Bahamas Bahrain Bangladesh Barbados Belarus Belgium Belize Benin Bermuda Bolivia Bosnia and Herzegovina Brazil Brunei Bulgaria Burma Cambodia Cameroon Canada Cayman Islands Chad Chile China Colombia Congo (Brazzaville) Congo (Kinshasa) Cook Islands Costa Rica Croatia Cyprus Czech Republic Denmark Djbouti Dominica Dominican Republic Egypt El Salvador Equatorial Guinea Ethiopia Eritrea Estonia Fiji Finland France French Pacific Islands French Guiana Gabon Georgia, Republic of Germany Ghana Gibraltar Greece Greenland Grenada Guadeloupe Guatemala Guinea Guyana Haiti Honduras Hong Kong Hungary Iceland India Indonesia Ireland Israel Italy Ivory Coast Jamaica Japan Jordan Kazakhstan Kenya Korea, South Kutubu Kyrgyzstan Latvia Lebanon Liberia Lithuania Macau S.A.R. Macedonia Madagascar Malaysia Maldives Mali Malta Marshall Islands Mauritania Mauritius Mexico Micronesia, Federated States of Midway Islands Moldova Monaco Mongolia Montenegro Montserrat Morocco Mozambique Namibia Nepal Netherlands Netherlands Antilles New Caledonia New Zealand Nicaragua Niger Niue Norway Oman Pakistan Panama Papau New Guinea Paracel Islands Paraguay Peru Philippines Poland Portugal Puerto Rico Romania Russia St. Kitts and Nevis St. Lucia St. Pierre and Miquelon St. Vincent and the Grenadines Samoa San Marino Senegal Serbia and Montenegro Sierra Leone Singapore Slovakia Slovenia South Africa Spain Spratly Islands Sri Lanka Suriname Swaziland Sweden Switzerland Syria Taiwan Tanzania Thailand Togo Tonga Trinidad and Tobago Tunisia Turkey Turkmenistan Turks and Caicos Islands Uganda Ukraine United Kingdom Uruguay Uzbekistan Vanuatu Vietnam Virgin Islands (British) Virgin Islands (U.S.) Yemen Yugoslavia Other Non OPEC Period-Unit: Monthly-Thousand Barrels per Day Annual-Thousand Barrels per Day

59

Glacial-Interglacial Changes in Moisture Sources for Greenland: Influences on the Ice Core Record of Climate  

Science Journals Connector (OSTI)

...why the average amplitude of the 8180 shifts in the Camp Century ice core (north-west Greenland) is much larger than...the different ice cores. The issue of what sets the Camp Century core apart-including arguments for and against ice...

C. D. Charles; D. Rind; J. Jouzel; R. D. Koster; R. G. Fairbanks

1994-01-28T23:59:59.000Z

60

Changes in sea-level associated with modifications on the mass balance of the Greenland and Antartic ice sheets over the 21st century  

E-Print Network (OSTI)

Changes in runoff from Greenland and Antarctica are often cited as one of the major concerns linked to anthropogenic changes in climate. The changes in mass balance, and associated changes in sea-level, of these two ice ...

Bugnion, Vronique.

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61

The Holocene sedimentary history of the Kangerlussuaq Fjord-valley fill, West Greenland  

Science Journals Connector (OSTI)

West Greenland has been intensively studied to reconstruct and better understand past relative sea level changes and deglacial history. This study extends these efforts by linking sea level and deglacial history to the sedimentary infill successions of Kangerlussuaq Fjord and associated landward valleys. Based on published and new land- and sea-based geophysical data, radiocarbon dates and geological observations we have characterized the infill and reconstructed the sedimentation history during the Holocene. Based on a revised sea level curve and data presented in this paper we defined three depositional phases. Phase I (>7000yrBP) is represented by dominant glaciomarine deposition associated with a tide-water glacier system. As the Greenland Ice Sheet (GIS) continued to retreat it became land based. During phase II (70001500yrBP) two separate depocenters formed. Keglen delta depocenter arose from a temporary stabilization phase of the GIS and prograded rapidly over the glaciomarine deposits of Phase I. Further inland, proglacial lake formation and subsequent sedimentary infill associated with the ongoing GIS retreat is represents the second depocenter. The Watson River connected both depocenters by a flood plain which transferred sediment from the GIS to the Keglen delta. Ongoing sea level fall due to glacio-isostastic uplift combined with a gradually cooler and dryer climate resulted in terrace formation along the Watson River flood plain. Around 4000yrBP, the GIS margin reached its most landward location and began to advance to its present location. The final phase (Phase III; <1500yrBP) is represented by a stabilized GIS position and a relative sea level rise which led to aggrading conditions near the present-day delta plain of Watson River. Simultaneously, subaqueous channels were formed at the delta front by hyperpycnal flows associated with jkulhlaup events.

Joep E.A. Storms; Ilja L. de Winter; Irina Overeem; Guy G. Drijkoningen; Holger Lykke-Andersen

2012-01-01T23:59:59.000Z

62

Meltwater flux and runoff modeling in the abalation area of jakobshavn Isbrae, West Greenland  

SciTech Connect

The temporal variability in surface snow and glacier melt flux and runoff were investigated for the ablation area of lakobshavn Isbrae, West Greenland. High-resolution meteorological observations both on and outside the Greenland Ice Sheet (GrIS) were used as model input. Realistic descriptions of snow accumulation, snow and glacier-ice melt, and runoff are essential to understand trends in ice sheet surface properties and processes. SnowModel, a physically based, spatially distributed meteorological and snow-evolution modeling system was used to simulate the temporal variability of lakobshavn Isbrre accumulation and ablation processes for 2000/01-2006/07. Winter snow-depth observations and MODIS satellite-derived summer melt observations were used for model validation of accumulation and ablation. Simulations agreed well with observed values. Simulated annual surface melt varied from as low as 3.83 x 10{sup 9} m{sup 3} (2001/02) to as high as 8.64 x 10{sup 9} m{sup 3} (2004/05). Modeled surface melt occurred at elevations reaching 1,870 m a.s.l. for 2004/05, while the equilibrium line altitude (ELA) fluctuated from 990 to 1,210 m a.s.l. during the simulation period. The SnowModel meltwater retention and refreezing routines considerably reduce the amount of meltwater available as ice sheet runoff; without these routines the lakobshavn surface runoff would be overestimated by an average of 80%. From September/October through May/June no runoff events were simulated. The modeled interannual runoff variability varied from 1.81 x 10{sup 9} m{sup 3} (2001/02) to 5.21 x 10{sup 9} m{sup 3} (2004/05), yielding a cumulative runoff at the Jakobshavn glacier terminus of {approx}2.25 m w.eq. to {approx}4.5 m w.eq., respectively. The average modeled lakobshavn runoff of {approx}3.4 km{sup 3} y{sup -1} was merged with previous estimates of Jakobshavn ice discharge to quantify the freshwater flux to Illulissat Icefiord. For both runoff and ice discharge the average trends are similar, indicating increasing (insignificant) influx of freshwater to the Illulissat Icefiord for the period 2000/01-2006/07. This study suggests that surface runoff forms a minor part of the overall Jakobshavn freshwater flux to the fiord: around 7% ({approx}3.4 km{sup 3} y{sup -1}) of the average annual freshwater flux of {approx}51.0 km{sup 3} y{sup -1} originates from the surface runoff.

Mernild, Sebastian Haugard [Los Alamos National Laboratory; Chylek, Petr [Los Alamos National Laboratory; Liston, Glen [COLORADO STATE UNIV.; Steffen, Konrad [UNIV OF COLORADO

2009-01-01T23:59:59.000Z

63

Revised estimates of Greenland ice sheet thinning histories based on ice-core records  

Science Journals Connector (OSTI)

Ice core records were recently used to infer elevation changes of the Greenland ice sheet throughout the Holocene. The inferred elevation changes show a significantly greater elevation reduction than those output from numerical models, bringing into question the accuracy of the model-based reconstructions and, to some extent, the estimated elevation histories. A key component of the ice core analysis involved removing the influence of vertical surface motion on the ?18O signal measured from the Agassiz and Renland ice caps. We re-visit the original analysis with the intent to determine if the use of more accurate land uplift curves can account for some of the above noted discrepancy. To improve on the original analysis, we apply a geophysical model of glacial isostatic adjustment calibrated to sea-level records from the Queen Elizabeth Islands and Greenland to calculate the influence of land height changes on the ?18O signal from the two ice cores. This procedure is complicated by the fact that ?18O contained in Agassiz ice is influenced by land height changes distant from the ice cap and so selecting a single location at which to compute the land height signal is not possible. Uncertainty in this selection is further complicated by the possible influence of Innuitian ice during the early Holocene (128kaBP). Our results indicate that a more accurate treatment of the uplift correction leads to elevation histories that are, in general, shifted down relative to the original curves at GRIP, NGRIP, DYE-3 and Camp Century. In addition, compared to the original analysis, the 1-? uncertainty is considerably larger at GRIP and NGRIP. These changes reduce the data-model discrepancy reported by Vinther etal. (2009) at GRIP, NGRIP, DYE-3 and Camp Century. A more accurate treatment of isostasy and surface loading also acts to improve the data-model fits such that the residuals at all four sites for the period 8kaBP to present are significantly reduced compared to the original analysis. Prior to 8kaBP, the possible influence of Innuitian ice on the inferred elevation histories prevents a meaningful comparison.

Benoit S. Lecavalier; Glenn A. Milne; Bo M. Vinther; David A. Fisher; Arthur S. Dyke; Matthew J.R. Simpson

2013-01-01T23:59:59.000Z

64

A LEKID-based CMB instrument design for large-scale observations in Greenland  

E-Print Network (OSTI)

We present the results of a feasibility study, which examined deployment of a ground-based millimeter-wave polarimeter, tailored for observing the cosmic microwave background (CMB), to Isi Station in Greenland. The instrument for this study is based on lumped-element kinetic inductance detectors (LEKIDs) and an F/2.4 catoptric, crossed-Dragone telescope with a 500 mm aperture. The telescope is mounted inside the receiver and cooled to $refrigerator to reduce background loading on the detectors. Linearly polarized signals from the sky are modulated with a metal-mesh half-wave plate that is rotated at the aperture stop of the telescope with a hollow-shaft motor based on a superconducting magnetic bearing. The modular detector array design includes at least 2300 LEKIDs, and it can be configured for spectral bands centered on 150~GHz or greater. Our study considered configurations for observing in spectral bands centered on 150, 210 and 267~GHz. The entire polarimeter is mounte...

Araujo, D C; Bond, J R; Bradford, K J; Chapman, D; Che, G; Day, P K; Didier, J; Doyle, S; Eriksen, H K; Flanigan, D; Groppi, C E; Hillbrand, S N; Johnson, B R; Jones, G; Limon, M; Miller, A D; Mauskopf, P; McCarrick, H; Mroczkowski, T; Reichborn-Kjennerud, B; Smiley, B; Sobrin, J; Wehus, I K; Zmuidzinas, J

2014-01-01T23:59:59.000Z

65

Numerical modelling of the energy balance and the englacial temperature of the Greenland Ice Sheet. Calculations for the ETH-Camp location (West Greenland, 1155 m a.s.l.)  

Science Journals Connector (OSTI)

In the present work, a numerical model that calculates the surface energy blance, mass balance and temperature in the uppermost 25 m of ice at a single location on a glacier is presented. The model is forced by five basic meteorological elements: air temperature and humidity, wind speed, cloud amount and precipitation. The model was developed for studies of the Greenland Ice Sheet. Parameterizations of the surface energy fluxes were optimised with data mainly from the ETH Camp, West Greenland (1155 m a.s.l.). The model was tested on data collected during the summer of 1990 in the ETH Camp. In this case measurements of the radiative fluxes could be used. A reasonable fit between measurements and calculations of mass balance and englacial temperature could be obtained. The energy balance of this summer is discussed. In a second application, the annual cycle of the energy and mass balance and the englacial temperature at the location of the ETH Camp was simulated. In this case long term average values of the input variables were estimated from measurements at other locations and the radiative fluxes were computed with the parameterizations. The effect of model uncertainties on the calculated mass balance and 10 m ice temperature is discussed. The energy balance and the relation between air and ice temperature are analysed. The uncertainty in the calculated ablation is so large (5001000 mm w.e./yr) that the contribution of ablation on the Greenland Ice Sheet to sea-level rise cannot be calculated with sufficient accuracy (i.e. 60 mm w.e./yr) with this kind of model. However, the model should be appropriate for the determination of the sensitivity of ablation to climate change. It is predicted that at the ETH Camp the mass balance will decrease by 610 mm w.e./yr after a temperature increase of 1C.

Wouter Greuell; Thomas Konzelmann

1994-01-01T23:59:59.000Z

66

Caribbean-GTZ Renewable Energy Program | Open Energy Information  

Open Energy Info (EERE)

Caribbean-GTZ Renewable Energy Program Caribbean-GTZ Renewable Energy Program Jump to: navigation, search Logo: Caribbean-GTZ Renewable Energy Program Name Caribbean-GTZ Renewable Energy Program Agency/Company /Organization Deutsche Gesellschaft für Internationale Zusammenarbeit (GIZ) GmbH Partner German Federal Ministry for Economic Cooperation and Development (BMZ) Sector Energy Topics Background analysis, Policies/deployment programs Website http://www.gtz.de/en/praxis/95 Country Antigua & Barbuda, Aruba, Bahamas, Barbados, Cayman Islands, Cuba, Dominica, Dominican Republic, Grenada, Guadeloupe, Haiti, Jamaica, Martinique, Puerto Rico, Saint Barthelemy, St. Kitts & Nevis, St. Lucia, St. Vincent and the Grenadines, Trinidad & Tobago, Turks & Caicos Islands, United States

67

A new ice thickness and bedrock data set for the Greenland ice sheet. R.L. Layberry, J.L. Bamber,  

E-Print Network (OSTI)

combined with data collected by the Technical University of Denmark in the 1970's to produce a new iceA new ice thickness and bedrock data set for the Greenland ice sheet. R.L. Layberry, J.L. Bamber of Kansas, Lawrence, KS 66045, 785/864-2700, U.S. Abstract - Ice thickness data collected between 1993

Kansas, University of

68

Age of the Fjord Stade moraines in the Disko Bugt region, western Greenland, and the 9.3 and 8.2 ka cooling events  

E-Print Network (OSTI)

warming and cooling, whereas the comparatively low-flux sector of the ice sheet in southeastern Disko Bugt cooling events Nicolás E. Young a,*, Jason P. Briner a , Dylan H. Rood b,c , Robert C. Finkel d , Lee B 2012 Accepted 17 September 2012 Available online Keywords: Greenland Ice Sheet Moraines 10 Be exposure

Briner, Jason P.

69

Sea Level Rise, Green Greenland & Fantabulous Inference To be removed from Jim Hansen's e-mail list respond to sender with REMOVE as subject  

E-Print Network (OSTI)

Sea Level Rise, Green Greenland & Fantabulous Inference To be removed from Jim Hansen's e-mail list respond to sender with REMOVE as subject Sea Level Rise: I confess to collaborating with Michael Le Page in making an abbreviated version of "Scientific reticence and sea level rise" http

Hansen, James E.

70

Greenland ice sheet surface mass-balance variability: 19912003 Byrd Polar Research Center, The Ohio State University, 1090 Carmack Road, Columbus, OH 43210-1002, USA  

E-Print Network (OSTI)

Greenland ice sheet surface mass-balance variability: 1991­2003 J.E. BOX Byrd Polar Research Center. There is little evidence for a total ice-sheet surface mass-balance trend, although the meltwater runoff has a positive trend and, combined with iceberg discharge and basal melting estimates, suggests the ice sheet

Box, Jason E.

71

Greenland ice sheet surface mass-balance modeling in a 131-year perspective, 1950-2080  

SciTech Connect

Fluctuations in the Greenland Ice Sheet (GrIS) surface mass-balance (SMB) and freshwater influx to the surrounding oceans closely follow climate fluctuations and are of considerable importance to the global eustatic sea level rise. SnowModel, a state-of-the-art snow-evolution modeling system, was used to simulate variations in the GrIS melt extent, surface water balance components, changes in SMB, and freshwater influx to the ocean. The simulations are based on the IPCC scenario AlB modeled by the HIRHAM4 RCM (using boundary conditions from ECHAM5 AOGCM) from 1950 through 2080. In-situ meteorological station (GC-Net and WMO DMI) observations from inside and outside the GrIS were used to validate and correct RCM output data before it was used as input for SnowModel. Satellite observations and independent SMB studies were used to validate the SnowModel output and confirm the model's robustness. We simulated a {approx}90% increase in end-of-summer surface melt extent (0.483 x 10{sup 6} km{sup 2}) from 1950 to 2080, and a melt index (above 2,000-m elevation) increase of 138% (1.96 x 10{sup 6} km{sup 2} x days). The greatest difference in melt extent occured in the southern part of the GrIS, and the greatest changes in the number of melt days was seen in the eastern part of the GrIS ({approx}50-70%) and was lowest in the west ({approx}20-30%). The rate of SMB loss, largely tied to changes in ablation processes, lead to an enhanced average loss of 331 km{sup 3} from 1950 to 2080, an average 5MB level of -99 km{sup 3} for the period 2070-2080. GrIS surface freshwater runoff yielded an eustatic rise in sea level from 0.8 {+-} 0.1 (1950-1959) to 1.9 {+-} 0.1 mm (2070-2080) sea level equivalent (SLE) y{sup -1}. The accumulated GrIS freshwater runoff contribution from surface melting equaled 160 mm SLE from 1950 through 2080.

Mernild, Sebastian Haugard [Los Alamos National Laboratory; Liston, Glen [COLORADO STATE UNIV.; Hiemstra, Christopher [COLORADO STATE UNIV.; Christensen, Jens [DANISH METEOROLOGICAL INS.

2009-01-01T23:59:59.000Z

72

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EETD NEWSLETTER - MANAGE SUBSCRIPTIONS EETD NEWSLETTER - MANAGE SUBSCRIPTIONS (red fields are required) Manage subscriptions: Subscribe Unsubscribe Name E-Mail Affiliation Address Address (line 2) City State/Province Zip/Postal Code Country (please select a country) none Afghanistan Albania Algeria American Samoa Andorra Angola Anguilla Antarctica Antigua and Barbuda Argentina Armenia Aruba Australia Austria Azerbaijan Bahamas Bahrain Bangladesh Barbados Belarus Belgium Belize Benin Bermuda Bhutan Bolivia Bosnia and Herzegowina Botswana Bouvet Island Brazil British Indian Ocean Territory Brunei Darussalam Bulgaria Burkina Faso Burundi Cambodia Cameroon Canada Cape Verde Cayman Islands Central African Republic Chad Chile China Christmas Island Cocos (Keeling) Islands Colombia Comoros Congo Congo, the Democratic Republic of the Cook Islands Costa Rica Cote d'Ivoire Croatia (Hrvatska) Cuba Cyprus Czech Republic Denmark Djibouti Dominica Dominican Republic East Timor Ecuador Egypt El Salvador Equatorial Guinea Eritrea Estonia Ethiopia Falkland Islands (Malvinas) Faroe Islands Fiji Finland France France, Metropolitan French Guiana French Polynesia French Southern Territories Gabon Gambia Georgia Germany Ghana Gibraltar Greece Greenland Grenada Guadeloupe Guam Guatemala Guinea Guinea-Bissau Guyana Haiti Heard and Mc Donald Islands Holy See (Vatican City State) Honduras Hong Kong Hungary Iceland India Indonesia Iran (Islamic Republic of) Iraq Ireland Israel Italy Jamaica Japan Jordan Kazakhstan Kenya Kiribati Korea, Democratic People's Republic of Korea, Republic of Kuwait Kyrgyzstan Lao People's Democratic Republic Latvia Lebanon Lesotho Liberia Libyan Arab Jamahiriya Liechtenstein Lithuania Luxembourg Macau Macedonia, The Former Yugoslav Republic of Madagascar Malawi Malaysia Maldives Mali Malta Marshall Islands Martinique Mauritania Mauritius Mayotte Mexico Micronesia, Federated States of Moldova, Republic of Monaco Mongolia Montserrat Morocco Mozambique Myanmar Namibia Nauru Nepal Netherlands Netherlands Antilles New Caledonia New Zealand Nicaragua Niger Nigeria Niue Norfolk Island Northern Mariana Islands Norway Oman Pakistan Palau Panama Papua New Guinea Paraguay Peru Philippines Pitcairn Poland Portugal Puerto Rico Qatar Reunion Romania Russian Federation Rwanda Saint Kitts and Nevis Saint LUCIA Saint Vincent and the Grenadines Samoa San Marino Sao Tome and Principe Saudi Arabia Senegal Seychelles Sierra Leone Singapore Slovakia (Slovak Republic) Slovenia Solomon Islands Somalia South Africa South Georgia and the South Sandwich Islands Spain Sri Lanka St. Helena St. Pierre and Miquelon Sudan Suriname Svalbard and Jan Mayen Islands Swaziland Sweden Switzerland Syrian Arab Republic Taiwan, Province of China Tajikistan Tanzania, United Republic of Thailand Togo Tokelau Tonga Trinidad and Tobago Tunisia Turkey Turkmenistan Turks and Caicos Islands Tuvalu Uganda Ukraine United Arab Emirates United Kingdom United States United States Minor Outlying Islands Uruguay Uzbekistan Vanuatu Venezuela Viet Nam Virgin Islands (British) Virgin Islands (U.S.) Wallis and Futuna Islands Western Sahara Yemen Yugoslavia Zambia Zimbabwe

73

Characterization of U/Pu Particles Originating From the Nuclear Weapon Accidents at Palomares, Spain, 1966 And Thule, Greenland, 1968  

SciTech Connect

Following the USAF B-52 bomber accidents at Palomares, Spain in 1966 and at Thule, Greenland in 1968, radioactive particles containing uranium (U) and plutonium (Pu) were dispersed into the environment. To improve long-term environmental impact assessments for the contaminated ecosystems, particles from the two sites have been isolated and characterized with respect to properties influencing particle weathering rates. Low [239]Pu/[235]U (0.62-0.78) and [240]Pu/[239]Pu (0.055-0.061) atom ratios in individual particles from both sites obtained by Inductively Coupled Plasma Mass Spectrometry (ICP-MS) show that the particles contain highly enriched U and weapon-grade Pu. Furthermore, results from electron microscopy with Energy Dispersive X-ray analysis (EDX) and synchrotron radiation (SR) based micrometer-scale X-ray fluorescence ({micro}-XRF) 2D mapping demonstrated that U and Pu coexist throughout the 1-50 {micro}m sized particles, while surface heterogeneities were observed in EDX line scans. SR-based micrometer-scale X-ray Absorption Near Edge Structure Spectroscopy ({micro}-XANES) showed that the particles consisted of an oxide mixture of U (predominately UO[2] with the presence ofU[3][8]) and Pu ((III)/(IV), (V)/(V) or (III), (IV) and (V)). Neither metallic U or Pu nor uranyl or Pu(VI) could be observed. Characteristics such as elemental distributions, morphology and oxidation states are remarkably similar for the Palomares and Thule particles, reflecting that they originate from similar source and release scenarios. Thus, these particle characteristics are more dependent on the original material from which the particles are derived (source) and the formation of particles (release scenario) than the environmental conditions to which the particles have been exposed since the late 1960s.

Lind, O.C.; Salbu, B.; Janssens, K.; Proost, K.; Garcia-Leon, M.; Garcia-Tenorio, R.

2007-07-10T23:59:59.000Z

74

The influence of air temperature inversions on snowmelt and glacier mass-balance simulations, Ammassalik island, SE Greenland  

SciTech Connect

In many applications, a realistic description of air temperature inversions is essential for accurate snow and glacier ice melt, and glacier mass-balance simulations. A physically based snow-evolution modeling system (SnowModel) was used to simulate eight years (1998/99 to 2005/06) of snow accumulation and snow and glacier ice ablation from numerous small coastal marginal glaciers on the SW-part of Ammassalik Island in SE Greenland. These glaciers are regularly influenced by inversions and sea breezes associated with the adjacent relatively low temperature and frequently ice-choked fjords and ocean. To account for the influence of these inversions on the spatiotemporal variation of air temperature and snow and glacier melt rates, temperature inversion routines were added to MircoMet, the meteorological distribution sub-model used in SnowModel. The inversions were observed and modeled to occur during 84% of the simulation period. Modeled inversions were defined not to occur during days with strong winds and high precipitation rates due to the potential of inversion break-up. Field observations showed inversions to extend from sea level to approximately 300 m a.s.l., and this inversion level was prescribed in the model simulations. Simulations with and without the inversion routines were compared. The inversion model produced air temperature distributions with warmer lower elevation areas and cooler higher elevation areas than without inversion routines due to the use of cold sea-breeze base temperature data from underneath the inversion. This yielded an up to 2 weeks earlier snowmelt in the lower areas and up to 1 to 3 weeks later snowmelt in the higher elevation areas of the simulation domain. Averaged mean annual modeled surface mass-balance for all glaciers (mainly located above the inversion layer) was -720 {+-} 620 mm w.eq. y{sup -1} for inversion simulations, and -880 {+-} 620 mm w.eq. y{sup -1} without the inversion routines, a difference of 160 mm w.eq. y{sup -1}. The annual glacier loss for the two simulations was 50.7 x 10{sup 6} m{sup 3} y{sup -1} and 64.4 x 10{sup 6} m{sup 3} y{sup -1} for all glaciers - a difference of {approx}21%. The average equilibrium line altitude (ELA) for all glaciers in the simulation domain was located at 875 m a.s.l. and at 900 m a.s.l. for simulations with or without inversion routines, respectively.

Mernild, Sebastian Haugard [Los Alamos National Laboratory; Liston, Glen [COLORADO STATE UNIV.

2009-01-01T23:59:59.000Z

75

Increasing runoff and sediment load from the Greenland ice sheet at kangerlussuaq (Sonder Stromfjord) in a 30-year perspective, 1979-2008  

SciTech Connect

This observation and modeling study provides insights into runoff and sediment load exiting the Watson River drainage basin, Kangerlussuaq, West Greenland during a 30 year period (1978/79-2007/08) when the climate experienced increasing temperatures and precipitation. The 30-year simulations quantify the terrestrial freshwater and sediment output from part of the Greenland Ice Sheet (GrIS) and the land between the GrIS and the ocean, in the context of global warming and increasing GrIS surface melt. We used a snow-evolution modeling system (SnowModel) to simulate the winter accumulation and summer ablation processes, including runoff and surface mass balance (SMB), of the Greenland ice sheet. Observed sediment concentrations were related to observed runoff, producing a sediment-load time series. To a large extent, the SMB fluctuations could be explained by changes in net precipitation (precipitation minus evaporation and sublimation), with 8 out of 30 years having negative SMB, mainly because of relatively low annual net precipitation. The overall trend in net precipitation and runoff increased significantly, while 5MB increased insignificantly throughout the simulation period, leading to enhanced precipitation of 0.59 km{sup 3} w.eq. (or 60%), runoff of 0.43 km{sup 3} w.eq (or 54%), and SMB of 0.16 km3 w.eq. (or 86%). Runoff rose on average from 0.80 km{sup 3} w.eq. in 1978/79 to 1.23 km{sup 3} w.eq. in 2007/08. The percentage of catchment oudet runoff explained by runoff from the GrIS decreased on average {approx} 10%, indicating that catchment runoff throughout the simulation period was influenced more by precipitation and snowmelt events, and less by runoff from the GrIS. Average variations in the increasing Kangerlussuaq runoff from 1978/79 through 2007/08 seem to follow the overall variations in satellite-derived GrIS surface melt, where 64% of the variations in simulated runoff were explained by regional melt conditions on the GrIS. Throughout the simulation period, the sediment load varied from a minimum of 0.96 x 10{sup 6} t y{sup -1} in 1991/92 to a maximum of 3.52 x 10{sup 6} t y{sup -1} in 2006/07, showing an average increase of sediment load of 9.42 x 10{sup 5} t (or 72%) throughout the period.

Mernild, Sebastian Haugard [Los Alamos National Laboratory; Liston, Glen [COLORADO STATE UNIV.; Hasholt, Bent [UNIV OF COPENGAGEN; Steffen, Konrad [UNIV OF COLORADO; Van Den Broeke, Michiel [UTRECHT UNIV; Mcgrath, Daniel [UNIV OF COLORADO; Yde, Jacob [UNIV OF AARHUS

2009-01-01T23:59:59.000Z

76

Generation of a novel 1km NDVI data set over Canada, the northern United States, and Greenland based on historical AVHRR data  

Science Journals Connector (OSTI)

Time series of the Normalized Difference Vegetation Index (NDVI) derived from satellite observations provide important information on the state of terrestrial vegetation over a wide range of spatiotemporal scales. For understanding long-term changes in terrestrial ecosystems (post-1981), data collected by the Advanced Very High Resolution Radiometer (AVHRR) on board the satellites of National Oceanic and Atmospheric Administration (NOAA) series is a unique source of information. In this paper, we describe a new processing methodology for a comprehensive AVHRR data set at 1km spatial resolution acquired over Canada, the northern United States and Greenland post-1981. The methodology incorporates a pre-processing algorithm, Canadian AVHRR Processing System (CAPS), recently developed by the Canada Centre of Remote Sensing (CCRS), which enables highly accurate geolocation and ortho-rectification at efficiency rates of >90%. Once image navigation is completed, our approach consists of five key steps: first, two clear-sky composites for each 10day interval are generated from the forward or backward scattering hemisphere; second, AVHRR Channel 1 and 2 reflectances are normalized to the AVHRR/3 on board NOAA-17 to account for differences in the spectral response function among the AVHRR sensors; third, atmospheric correction is performed using the Simplified Method for Atmospheric correction (SMAC) algorithm, using standard meteorological data sets (water vapor, surface level air pressure, ozone); fourth, NDVI is calculated based on atmospherically corrected Channel 1 and 2 reflectances; and finally, the NDVI is adjusted for directional effects based on the Ross-Thick Li-Sparse Bidirectional Reflectance Distribution Function (BRDF) model. The processed NDVI data are compared to an equivalent spatially and temporally overlapping MODIS NDVI data set from 2001 to 2005 for validation. Results at continental scale indicate that time series of MODIS and AVHRR were similar for a wide range of biomes and generalized ecoregions. Analysis stratified by land cover indicated that the correlation was strongest for homogeneous land cover types, such as cropland, when compared to structurally more diverse classes, such as deciduous broadleaf forests. The comparison of the NDVI at the local scale at seven sites of the Fluxnet Canada Research Network resulted in the correlation coefficient r=0.95. Given confidence in the processing approach, this NDVI data set can be a valuable source of information for climate and vegetation-related studies over Canada and the northern United States.

Fabio M.A. Fontana; Nicholas C. Coops; Konstantin V. Khlopenkov; Alexander P. Trishchenko; Michael Riffler; Michael A. Wulder

2012-01-01T23:59:59.000Z

77

Recent Changes in Greenland & Antarctica  

E-Print Network (OSTI)

lake drainage her height ?5 = old water level Lake used to be 8m (24 ft) deep Flow rate Niagara Falls depth: Volume of water in lake over time Field project: If meltwater reaches the bed, does it affect ice the ability to make accurate projections (IPCC, 2007). From ice sheets /glaciers: 0.04 to 0.23 meters #12;IPCC

Bitz, Cecilia

78

Greenland mass balance from GRACE  

E-Print Network (OSTI)

and Sci. , Sioux Falls, S. D. Peltier, W. R. (1996), MantleScience, 273, 1359 1364. Peltier, W. R. (2004), GlobalTushingham, A. M. , and W. R. Peltier (1991), ICE-3G: A new

Velicogna, Isabella; Wahr, John

2005-01-01T23:59:59.000Z

79

Crustal structure of Guadeloupe Islands and the Lesser Antilles Arc from a new gravity and magnetic synthesis  

E-Print Network (OSTI)

the compilation and processing of available, on-land, airborne and marine, gravity and magnetic data acquired is associated with formations consistent with the low measured density and the underlying hydrothermal system

Paris-Sud XI, Université de

80

A new bed elevation dataset for Greenland  

E-Print Network (OSTI)

ice penetrating radar (IPR) systems. As a consequence, wefrom a number of airborne IPR missions have been col- lated,added for years between the IPR acquisition date and the

2013-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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

International Student and Scholar Enrollment & Statistical Report  

E-Print Network (OSTI)

Suriname 1 Ghana 18 Swaziland 1 Greece 19 Sweden 8 Grenada 1 Switzerland 8 Guatemala 21 Syria 4 Guyana 2

Ginzel, Matthew

82

Amrique latine et Carabes  

E-Print Network (OSTI)

P?ROU ?QUATEUR COLOMBIE VENEZUELA GUYANA SURINAME GUYANE FRAN?AISE MEXIQUE MARTINIQUE GUADELOUPE SAINT

83

POPULATION DENSITY, 2000 Population density measures the number  

E-Print Network (OSTI)

´ GUADELOUPE 0 25 50 km NETHERLAND ANTILLES NETHERLAND ANTILLES ST. KITTS NEVIS Copyright 2009. The Trustees

Columbia University

84

Greenland Ice Sheet "Sliding" a Small Contributor to Future Sea...  

Office of Science (SC) Website

(ice2sea manuscript no. 121). ElmerIce simulations were performed using high-performance computing resources from Grand quipement National de Calcul Intensif - Centre...

85

ICE CORES | History of Research, Greenland and Antarctica  

Science Journals Connector (OSTI)

Abstract Ice samples collected from polar ice sheets have been used to study past climate changes going almost as far back as 1My. The first ice core projects in the 1960s identified major climate transitions. Subsequent projects have shown that abrupt climate changes have occurred many times in the past and that there is a close link between high levels of atmospheric carbon dioxide and warm climate conditions.

M. Aydin

2013-01-01T23:59:59.000Z

86

ICE CORES | History of Research, Greenland and Antarctica  

Science Journals Connector (OSTI)

Ice samples collected from the polar ice sheets have been used to study past climate changes during the last million years. The first ice-core projects in the 1960s identified the major climate periods. Subsequent projects have shown that abrupt climate changes have occurred many times in the past and that there is a close link between high levels of atmospheric carbon dioxide and warm climate conditions.

K. Taylor

2007-01-01T23:59:59.000Z

87

Greenland temperature response to climate forcing during the last deglaciation  

Science Journals Connector (OSTI)

...quascirev.2006.08.002 63 Gundestrup N. S. Dahl-Jensen D. Hansen B. L. Kelty J. , Bore-hole survey at Camp Century, 1989 . Cold Reg. Sci. Technol. 21 , 187 193 ( 1993 ). 10.1016/0165-232X(93)90006-T 64 Buizert...

Christo Buizert; Vasileios Gkinis; Jeffrey P. Severinghaus; Feng He; Benoit S. Lecavalier; Philippe Kindler; Markus Leuenberger; Anders E. Carlson; Bo Vinther; Valrie Masson-Delmotte; James W. C. White; Zhengyu Liu; Bette Otto-Bliesner; Edward J. Brook

2014-09-05T23:59:59.000Z

88

Surface Wave Dispersion and Crust Structure in Greenland  

Science Journals Connector (OSTI)

......s-', the S-velocity of 1.94 kms-l and the density of 0.91 g ~ m - ~ were taken from the deep drilling of Camp Century, 200 km east of Thule (Smith 1965). The velocities are in good agreement with those found by Holtzscherer (1954......

Sren Gregersen

1971-01-01T23:59:59.000Z

89

Mercury in the Greenland Ice Sheet: Further Data  

Science Journals Connector (OSTI)

...ed from two separate sites (Camp Century and a "virgin site"), they...analyzed ice core samples from Camp Century (770 1O'N, 61008'W) and...Date Mercury (in) (ng/liter) Camp Century 56.94 1850 13 10 Site 2 54...

Roderick A. Carr; Peter E. Wilkniss

1973-08-31T23:59:59.000Z

90

Icelandic Geothermal Activity and the Mercury of the Greenland Icecap  

Science Journals Connector (OSTI)

... sites in Iceland during June and July 1972. Field air sampling procedures and analyses by flameless atomic absorption were carried out as described in the Hawaiian study.

B. Z. SIEGEL; S. M. SIEGEL; F. THORARINSSON

1973-02-23T23:59:59.000Z

91

Anthropogenic Chlorofluoromethanes in the Greenland and Norwegian Seas  

Science Journals Connector (OSTI)

...that are younger than the Bonneville shoreline (5). The scarps...year calculated for the Bonneville shore-line yields an age...Ed. (Federal Aviation Administration, Washington, D.C., 1980...moderate-ly high resolving power, show weak at-mospheric...

J. L. BULLISTER; R. F. WEISS

1983-07-15T23:59:59.000Z

92

Paleofluvial Mega-Canyon Beneath the Central Greenland Ice Sheet  

Science Journals Connector (OSTI)

...m km ?1 , which is similar to the southern 500 km of the Colorado River and around three times larger than the average for the Mississippi...Fowler A. C. Clark C. D. Hulton N. R. J. , Subglacial floods beneath ice sheets . Phil. Trans. R. Soc. A 364 , 1769...

Jonathan L. Bamber; Martin J. Siegert; Jennifer A. Griggs; Shawn J. Marshall; Giorgio Spada

2013-08-30T23:59:59.000Z

93

Complex systems influence melting of Greenland ice sheet  

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

methane levels three times larger than expected over Four Corners region Probing Fukushima with cosmic rays should help speed cleanup of damaged plant Dark spaces could change...

94

Coherent radar ice thickness measurements over the Greenland ice sheet  

E-Print Network (OSTI)

systems are designed to use pulse compression techniques and coherent integration to obtain the high sensitivity required to measure the thickness of more than 4 km of cold ice. We used these systems to collect radar data over the interior and margins...

Gogineni, S. Prasad; Tammana, Dilip; Braaten, David A.; Leuschen, C.; Legarsky, J.; Kanagaratnam, P.; Stiles, J.; Allen, C.; Jezek, K.; Akins, T.

2001-12-27T23:59:59.000Z

95

Miniaturized Air to Refrigerant Heat Exchangers | Department...  

Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

- Grenada, MS -- International Copper Association - New York, NY -- Wieland - Ulm, Germany -- Heat Transfer Technologies - Abington, PA DOE Funding: 1,500,000 Cost Share: NA...

96

Heating, Ventilation, and Air Conditioning Projects | Department...  

Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

- Grenada, MS -- International Copper Association - New York, NY -- Wieland - Ulm, Germany -- Heat Transfer Technologies - Abington, PA Multi-Function Fuel-Fired Heat Pump...

97

World geothermal power generation in the period 2001-2005 | Open...  

Open Energy Info (EERE)

Costa Rica, France (Guadeloupe), Iceland,Indonesia, Italy1,Kenya, Mexico, Nicaragua, Russia, and the USA have increased the capacity of their powerplant installations by more...

98

World Geothermal Power Generation in the Period 2001-2005 | Open...  

Open Energy Info (EERE)

Costa Rica, France (Guadeloupe), Iceland, Indonesia, Italy1, Kenya, Mexico, Nicaragua, Russia, and the USA have increased the capacity of their power plant installations by more...

99

L'Amrique latine ou les Amriques latines Georges Couffignal  

E-Print Network (OSTI)

, le Suriname, la Guyane, la Jamaïque, la Guadeloupe, la Martinique et les mini ?tats de la Caraïbe. Au

Paris-Sud XI, Université de

100

14010651-6226-5013-257-124-6 OTHER ALLOCATIONS  

E-Print Network (OSTI)

FRENCH POLYNESIA BOLIVIABOLIVIA Gabon Zimbawe Sri LankaSri Lanka ArgentinaArgentina ColombieColombia Togo IndiaIndia Gabon Togo Guadeloupe Zimbawe EGYPTEGYPT TUNISIATUNISIAMOROCCOMOROCCO SENEGALSENEGAL

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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.


101

Proceedings World Geothermal Congress 2005 Antalya, Turkey, 24-29 April 2005  

E-Print Network (OSTI)

Proceedings World Geothermal Congress 2005 Antalya, Turkey, 24-29 April 2005 1 Geophysical Methods Applied to the Assessment of the Bouillante Geothermal Field (Guadeloupe, French West Indies) Hubert, 45064 Orléans Cedex 2, France h.fabriol@brgm.fr Keywords: geothermal exploration, Guadeloupe Island

Boyer, Edmond

102

Characterization of resistance to the Mexican spittlebug complex Aeneolamia albofasciata (Lallemand) and Prosapia simulans (Walker) in selected buffelgrass genotypes  

E-Print Network (OSTI)

- zuela, Guyana, Surinam, Trinidad, Tobago, Grenada, Brazil and Argen- tina. Borrer and DeLong (1976) placed the Homoptera among those insects that undergo incomplete metamorphosis. The spittlebug conforms, pass- ing through egg, nymph and adult stages...

Head, Henry Wesley

2012-06-07T23:59:59.000Z

103

History of Ancient Copper Smelting Pollution During Roman and Medieval Times Recorded in Greenland Ice  

Science Journals Connector (OSTI)

...1991), pp. 13-42. 27. Natural copper flux was calculated...fullerenes by searching for noble gases trapped inside the fullerene...correlation of C and trapped noble gas atoms in meteorites is well...contain several trapped noble gas components that have anomalous...

Sungmin Hong; Jean-Pierre Candelone; Clair C. Patterson; Claude F. Boutron

1996-04-12T23:59:59.000Z

104

Greenland temperature, climate change, and human society during the last 11,600 years  

E-Print Network (OSTI)

Albuquerque, N.M. Wiersma, A.P. , Renssen, H. , 2006. Model-Morrill and Jacobsen, 2005; Wiersma and Renssen, 2006). Thepaleo-evidence from Europe (Wiersma and Renssen, 2006), this

Kobashi, Takuro

2007-01-01T23:59:59.000Z

105

Two-hundred-year record of biogenic sulfur in a south Greenland ice core (20D)  

E-Print Network (OSTI)

DC, 450-458, 1989. Wallington, T. J. , R. Atkinson, A.M.1983; Grosjean, 1984; Wallington et ai. , 1986; Barnes et

Whung, P.-Y.; Saltzman, E. S; Spencer, M. J; Mayewski, P. A; Gundestrup, N.

1994-01-01T23:59:59.000Z

106

Carbon-14 production compared to oxygen isotope records from Camp Century, Greenland and Devon Island, Canada  

Science Journals Connector (OSTI)

Carbon-14 production rate variations that are not explainable by geomagnetic changes are thought to be in antiphase with solar activity and as such should be in antiphase with paleotemperature records or proxy te...

David Andrew Fisher

1982-01-01T23:59:59.000Z

107

16C Rapid Temperature Variation in Central Greenland 70,000 Years Ago  

Science Journals Connector (OSTI)

...thousand years. When these increases were discovered [in Camp Century ice (2)], it was not clear whether they reflected...thousand years. When these increases were discovered [in Camp Century ice (2)], it was not clear whether they reflected...

C. Lang; M. Leuenberger; J. Schwander; S. Johnsen

1999-10-29T23:59:59.000Z

108

Mercury and Lead in the Greenland Ice Sheet: A Reexamination of the Data  

Science Journals Connector (OSTI)

...symbols; *, inclined shaft at Camp Century; 0, virgin trench site. The...upwind (east-south-east) from Camp Century, which, in turn, was 210 km...virgin site, at the periphery of Camp Century, and at a location be-tween...

Edward M. Dickson; C. C. Patterson; H. V. Weiss; M. Koide; E. D. Goldberg

1972-08-11T23:59:59.000Z

109

Phylogenetic and Physiological Diversity of Microorganisms Isolated from a Deep Greenland Glacier Ice Core  

Science Journals Connector (OSTI)

...size reduction, condensation of the cytoplasm...microorganisms from the atmospheric airflow into...enhanced the recovery of the high-GC...the presence of water channels and...2003. Bacterial recovery from ancient...Reeve. 2000. Recovery and identification...glacial ice and water in Canadas High...

V. I. Miteva; P. P. Sheridan; J. E. Brenchley

2004-01-01T23:59:59.000Z

110

Constraining ice mass loss from Jakobshavn Isbr (Greenland) using InSAR-measured crustal uplift  

Science Journals Connector (OSTI)

......Similar to the differential atmospheric and ionospheric signals...Furuya M. , Wahr J., 2005. Water level changes at an ice-dammed...Engineering a 2D quality mesh generator and Delaunay triangulator...A., Hensley S., 1997. Atmospheric effects in interferometric......

Lin Liu; John Wahr; Ian Howat; Shfaqat Abbas Khan; Ian Joughin; Masato Furuya

2012-03-01T23:59:59.000Z

111

In the Greenland and Norwegian Seas, sea ice advanced farther south and persisted  

E-Print Network (OSTI)

at high latitudes, ice-age conditions were not so different from those of today, with global cooling was that the larger area of snow and ice produced a cooling feedback through increased reflection of solarenergy, which found considerable ice-age cooling off Peru and along the Equator10 . Although the aver- age

Kurapov, Alexander

112

Ineson, J. R. & Surlyk, F. (eds) 2003. The Jurassic of Denmark and Greenland.:  

Science Journals Connector (OSTI)

...established'. Great stuff and a real eye opener to the personalities...surrounded by dense housing estates with their attendant vandalism...Valuing the Resource: the Sustainable Ap-proach', was introduced...in Somerset has remained a sustainable resource despite two centuries...

Simon R. A. Kelly

113

Radioactive cesium from the Chernobyl accident in the Greenland Ice Sheet  

Science Journals Connector (OSTI)

...snowfall on 5 June, airborne concentrations of 134CS...If we assume that airborne concentrations at Dye...indicate calculated airborne concentrations great-er...therefore likely that a fraction of the measured radioactive...modeling of radioactivity releases from the Chernobyl event...

CI Davidson; Harrington JR; MJ Stephenson; MC Monaghan; J Pudykiewicz; WR Schell

1987-08-07T23:59:59.000Z

114

Spread of ice mass loss into northwest Greenland observed by GRACE and GPS  

E-Print Network (OSTI)

Science Program, Solid Earth and Natural Hazards Program, Terrestrial Hydrology Program, and by the NSF Office

Khan, Shfaqat Abbas; Wahr, John; Bevis, Michael; Velicogna, Isabella; Kendrick, Eric

2010-01-01T23:59:59.000Z

115

Field Metabolic Rate and PCB Adipose Tissue Deposition Efficiency in East Greenland Polar Bears Derived from  

E-Print Network (OSTI)

Environmental Protection Agency within the Danish Cooperation for Environment in the Arctic (DANCEA). The early, if the modelled CB153 deposition efficiency were 10%, adult polar bears would require six times more energy than/index_en.cfm, VP JNN VG. The research on contamination of ringed seals was funded by the Danish

Schierup, Mikkel Heide

116

Georadar-derived estimates of firn density in the percolation zone, western Greenland ice sheet  

E-Print Network (OSTI)

surface elevation [Holland et al., 2011] and can substantially influence mass balance calculations based

Howat, Ian M.

117

Evaluating Greenland glacial isostatic adjustment corrections using GRACE, altimetry and surface mass balance data.  

E-Print Network (OSTI)

Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA Department of Geology, University at Buffalo, Buffalo, NY, USA Institute for Marine and

Sutterley, T. C.; Velicogna, I.; Csatho, B.; van den Broeke, M.; Rezvan-Behbahani, S.; Babonis, G.

2014-01-01T23:59:59.000Z

118

Quaternary Science Reviews 22 (2003) 16311646 Greenland--Antarctic phase relations and millennial time-scale  

E-Print Network (OSTI)

, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, 54-1520, 77 Massachusetts Avenue of the observed Holocene variability in deep-sea cores is controlled by solar luminosity variations, which if true

Wunsch, Carl

119

Levoglucosan as a specific marker of fire events in Greenland snow  

E-Print Network (OSTI)

,6-anhydro-b-D-glucopyranose) as a source-specific proxy of past fire activity in snow pits and ice cores. Levoglucosan is unambiguously a degradation product derived from cellulose burning at temperatures greater than 300 8C and is widely used as a biomass burning marker in aerosol analyses. We analyse samples

Paris-Sud XI, Université de

120

Spread of ice mass loss into northwest Greenland observed by GRACE and GPS  

E-Print Network (OSTI)

Geophys. J. Int. , 171(2), Peltier, W. R. (2004), Globaland VM2 viscosity profile of [Peltier, 2004]) to removeand VM2 viscosity profile [Peltier, 2004]. These predicted

Khan, Shfaqat Abbas; Wahr, John; Bevis, Michael; Velicogna, Isabella; Kendrick, Eric

2010-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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.


121

Geophys. J. Int. (2002) 150, 198229 Greenland glacial history and local geodynamic consequences  

E-Print Network (OSTI)

. Tarasov and W. Richard Peltier Department of Physics, University of Toronto, Canada. E-mail: peltier relative sea level (RSL) histories (Peltier 1994, 1996, 1998) currently provide surface boundary conditions et al. 1997; Greve et al. 1998; Tarasov & Peltier 1997b, 1999) including recent investigations

Peltier, W. Richard

122

Evaluating Greenland glacial isostatic adjustment corrections using GRACE, altimetry and surface mass balance data.  

E-Print Network (OSTI)

J. Intl 171 497508 Peltier W R 2004 Annu. Rev. Earthof GIA models: (1) global (Peltier 2004) and (2) regionala layered approximation of the Peltier VM2 mantle viscosity

Sutterley, T. C.; Velicogna, I.; Csatho, B.; van den Broeke, M.; Rezvan-Behbahani, S.; Babonis, G.

2014-01-01T23:59:59.000Z

123

What do accumulation records of single ice cores in Greenland Traute Cruger  

E-Print Network (OSTI)

for Coastal Research, GKSS Research Centre, Geesthacht, Germany Hubertus Fischer Alfred Wegener Institute, GKSS Research Centre, Geesthacht, Germany Received 14 May 2004; revised 12 August 2004; accepted 8

Fischer, Hubertus

124

Acceleration of the contribution of the Greenland and Antarctic ice sheets to sea level rise  

E-Print Network (OSTI)

make a large sea?level rise contribu- tion, Geophys. Res.and Antarctic ice sheets to sea level rise E. Rignot, 1,2 I.ice sheets to sea level rise, Geophys. Res. Lett. , 38,

Rignot, E.; Velicogna, I.; van den Broeke, M. R; Monaghan, A.; Lenaerts, J. T. M

2011-01-01T23:59:59.000Z

125

Sensitive response of the Greenland Ice Sheet to surface melt drainage over soft bed  

E-Print Network (OSTI)

by detailed energy balance observations. The Cryosphere 6, 199-209, doi:doi:10.5194/tc-6-199-2012 (2012). ... by frictional and geothermal heating accumulates at the 136 bed over the course of winter and is released together with the first SGL drainage 137 events. With either one of these factors included, our model was able to reproduce the 138 2010 spring...

Bougamont, M H; Christoffersen,P.; Hubbard, A. L.; Fitzpatrick, A. A.; Doyle, S. H.; Carter, S. P.

2014-09-29T23:59:59.000Z

126

Radon-222, CO, CH4 and Continental Dust over the Greenland and Norwegian Seas  

Science Journals Connector (OSTI)

... The experiment was undertaken to investigate the relationships between these parameters and air mass trajectories. Radon (222Rn)-a radioactive rare gas emanating essentially from large continental land areas-and dust ... removed by coagulation and fallout or washed out by rain or fog, although comparison of radon level and dust data may be helpful in tracing the trajectory and mixing of air ...

R. E. LARSON; R. A. LAMONTAGNE; P. E. WILKNISS; W. I. WITTMANN

1972-12-08T23:59:59.000Z

127

Basal Drainage System Response to Increasing Surface Melt on the Greenland Ice Sheet  

Science Journals Connector (OSTI)

...2010-2011 (NASA DAAC at the National Snow and Ice Data Center, Boulder, CO, 2010). 30 Murray T. Clarke G. K. C. , Black-box modeling...002214309790152375 41 Clarke G. K. C. , Hydraulics of subglacial outburst floods: New insights from the Spring-Hutter formulation . J. Glaciol...

T. Meierbachtol; J. Harper; N. Humphrey

2013-08-16T23:59:59.000Z

128

Interglacial High Sea Levels and the Control of Greenland Ice by the Precession of the Equinoxes  

Science Journals Connector (OSTI)

...handling and treatment, several pieces of the foil which had been irradiated earlier with a known neon ion flux of solar wind energy were attached to the foil. One of these test pieces has been analyzed so far, and no losses within 10 percent have...

C. Emiliani

1969-12-19T23:59:59.000Z

129

Molecular cloning of Schistosoma mansoni egg cDNA clones of importance to host immune response  

E-Print Network (OSTI)

tropical and subtropical Africa, South America, especially in Egypt, Nalagasy, Arabia, Brazil, Venezunelaf Surinam, and Guayanaf and in several Caribbean islands, including Puerto Rico, the Dominican Republic, St. Lucia, Martinique, and Guadeloupe...

Chao, Hsu

2012-06-07T23:59:59.000Z

130

IRD/T. Jaffr IRD/M.Dukhan  

E-Print Network (OSTI)

PERUPERU FRENCH POLYNESIA FRENCH POLYNESIA BOLIVIABOLIVIA Gabon Zimbawe Sri LankaSri Lanka ArgentinaArgentina ColombieColombia Togo IndiaIndia Gabon Togo Guadeloupe Zimbawe EGYPTEGYPT TUNISIATUNISIAMOROCCOMOROCCO

131

Comparison of theoretical and observed temperature profiles in Devon Island ice cap, Canada  

Science Journals Connector (OSTI)

......theoretical temperature profiles of the Camp Century, Greenland, borehole J. geophys...theoretical temperature profiles of the Camp Century, Greenland, borehole J. geophys...Langway from the borehole at Camp Century, Greenland (Weertman 1968......

W. S. B. Paterson; G. K. C. Clarke

1978-12-01T23:59:59.000Z

132

COTA, GLENN F., WALKER O. SMITH, JR., AND B. GREG ...  

Science Journals Connector (OSTI)

Photosynthesis of Phaeocystis in the Greenland Sea. Abstract-During the spring bloom in the northern. Greenland Sea in 1989, Phaeocystis displayed pho-.

1999-12-20T23:59:59.000Z

133

Late quaternary sea levels in the Gulf of Mexico  

E-Print Network (OSTI)

-isotope measurements on an ice core from Camp Century, Greenland...-isotope measurements on an ice core from Camp Century, Greenland...

Lindau, Charles Wayne

2012-06-07T23:59:59.000Z

134

c811 D103.33:216 DateReq: 3/8/2004 5 Yes  

E-Print Network (OSTI)

Apr 7, 2004 ... Figure. 1. Laboratory and test apparatus at Camp Century, Greenland . ... Camp Century, Greenland, during the summer of 31;)64. This report...

135

Seasonally resolved Alpine and Greenland ice core records of anthropogenic HCl emissions over the 20th century  

E-Print Network (OSTI)

emissions, waste incineration, coal burning 1. Introduction [2] In addition to HNO3 and H2SO4, HCl biomass burning activity in western Europe. From 1925 to 1960 the HCl levels were slightly higher (3­9 ng g?1 ), mainly due to growing coal burning emissions in western Europe. In the late 1960s a sharp

Fischer, Hubertus

136

High-Resolution Monitoring of Internal Layers Over the Greenland Ice Sheet P. Kanagaratnam, S.P. Gogineni  

E-Print Network (OSTI)

been attributed to the melting of mountain glaciers among other causes. The mass balance of the glacial ice plays an important role in the rise of the Earth's sea level. A key variable in assessing the mass. Accumulation data are sparse, and there are large uncertainties in existing accumulation rate maps derived from

Kansas, University of

137

Airborne UHF Radar for Fine Resolution Mapping of Near Surface Accumulation Layers in Greenland and West Antarctica  

E-Print Network (OSTI)

............................................................................................................................. 1 1.1 MOTIVATION ............................................................................................................................................................ 1 1.2 DOCUMENT ORGANIZATION... .................................................................................................................................. 3 CHAPTER 2: BACKGROUND ................................................................................................................................ 3 2.1 PREVIOUS ACCUMULATION RADAR DEVELOPMENT...

Lewis, Cameron Scott

2010-11-01T23:59:59.000Z

138

Feasibility of reconstructing paleoatmospheric records of selected alkanes, methyl halides, and sulfur gases from Greenland ice cores  

E-Print Network (OSTI)

study of ethane and propane oxidation in the tropo- sphere,alkanes (ethane, C 2 H 6 ; propane, C 3 H 8 ; n-butane, n-Cfluid contamination. 4.1.2. Propane [ 24 ] Propane levels in

Aydin, M.; Williams, M. B; Saltzman, E. S

2007-01-01T23:59:59.000Z

139

A greener Greenland? Climatic potential and long-term constraints on future expansions of trees and shrubs  

Science Journals Connector (OSTI)

...frequently occurring, desiccating foehn wind events and sequences of unusual cold...The degree of damage due to dry foehn wind from the inland icecap can vary substantially with local topography and might necessitate...

2013-01-01T23:59:59.000Z

140

Enhanced basal lubrication and the contribution of the Greenland ice sheet to future sea-level rise  

Science Journals Connector (OSTI)

...Scientific Computing Research and Biological and Environmental Research programs. M...at the National Energy Research Scientific Computing...version 2.0 development and simulations...temperature and geothermal flux fields taken...

Sarah R. Shannon; Antony J. Payne; Ian D. Bartholomew; Michiel R. van den Broeke; Tamsin L. Edwards; Xavier Fettweis; Olivier Gagliardini; Fabien Gillet-Chaulet; Heiko Goelzer; Matthew J. Hoffman; Philippe Huybrechts; Douglas W. F. Mair; Peter W. Nienow; Mauro Perego; Stephen F. Price; C. J. P. Paul Smeets; Andrew J. Sole; Roderik S. W. van de Wal; Thomas Zwinger

2013-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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

Journal of Volcanology and Geothermal Research, 11(1981) 11--27 Elsevier Scientific Publishing Company, Amsterdam --Printed in Belgium  

E-Print Network (OSTI)

Camp Century, Greenland core. Microparticle increases of this magnitude can not be accounted for merely

Howat, Ian M.

142

Weather - climate interactions in the eastern Antilles and the 2013 Christmas storm  

Science Journals Connector (OSTI)

This study considers eastern Antilles (11-18N, 64-57W) weather and climate interactions in the context of the 2013 Christmas storm. This unseasonal event caused flash flooding in Grenada, St Vincent, St Lucia, Martinique and Dominica from 24-25 ...

Mark R. Jury

143

SocialAffairs E c o n o m i c &  

E-Print Network (OSTI)

Eradication." No study for building a green economy for sustainable development can be final and definitiveSocialAffairs E c o n o m i c & #12;Road Map on Building a Green Economy for Sustainable and Export Development of Grenada. The completion of this first Road Map on Building A Green Economy

Kammen, Daniel M.

144

Environmental Health Dedicated to the advancement of the environmental health professional Volume 73, No. 2 September 2010  

E-Print Network (OSTI)

of the coastal waters. The goal of the study described in our cover feature, "The Bacteriological Analysis and Health Risks in the Urban Estuary of St. George's Bay, Grenada, West Indies," was to determine potential Deployed to the World Trade Center and Pentagon: 2001

145

WeatherClimate Interactions in the Eastern Antilles and the 2013 Christmas Storm  

Science Journals Connector (OSTI)

This study considers eastern Antilles (1118N, 6457W) weather and climate interactions in the context of the 2013 Christmas storm. This unseasonal event caused flash flooding in Grenada, St. Vincent, St. Lucia, Martinique, and Dominica from ...

Mark R. Jury

2014-11-01T23:59:59.000Z

146

Drought and Precipitation Monitoring for Enhanced Integrated Water Resources Management in the Caribbean  

E-Print Network (OSTI)

Drought and Precipitation Monitoring for Enhanced Integrated Water Resources Management for water resource management in Jamaica, Grenada and Guyana. A key element to ensuring the success for Water Resources Management, McGill University, Macdonald Campus, 21111 Lakeshore Rd., Ste. Anne de

Barthelat, Francois

147

GEOPHYSICAL RESEARCH LETTERS, VOL. 25, NO. 21, PAGES 3951-3954, NOVEMBER 1, 1998 Present-day uplift patterns over Greenland from  

E-Print Network (OSTI)

temperature and melting. Pre- vious studies [Le Meur and Huybrechts, 1996; Tarasov and Peltier, 1997] show how Meur, 1996b; Peltier, 1974; Wu and Peltier, 1982; Spada et al., 1992] with a 3-D thermomechanical ice [Peltier, 1974; Wu and Peltier, 1982; Lam- beck et al., 1990; Spada et al., 1992]. Following the work

Huybrechts, Philippe

148

Detecting the thermal aureole of a magmatic intrusion in immature to mature sediments: a case study in the East Greenland Basin (73N)  

Science Journals Connector (OSTI)

......fraction: after air-drying (AD), ethylene-glycol (EG) and hydrazine (Hy) treatment...39Ar dating basaltic intrusions in TGS (Price et-al. 1997). Based on this, it...Sci. Lett. (2002) 194:343-358. Price S.P. , Brodie J., Whitham A.G......

Charles Aubourg; Isabelle Techer; Laurent Geoffroy; Norbert Clauer; Franois Baudin

2014-01-01T23:59:59.000Z

149

Are seasonal calving dynamics forced by buttressing from ice mlange or undercutting by melting? Outcomes from full-Stokes simulations of Store Gletscher, West Greenland  

E-Print Network (OSTI)

has been widespread and synchronous below 69? N, but largely absent at higher latitudes, where coastal water is much colder (Seale et al., 2011). This suggests that these glaciers are retreating in response to changes in the ocean25 system. Warmer... is our region of interest, extensive5 crevassing makes the implementation of temperature difficult. The ability of subglacial meltwater to penetrate upwards through basal crevasses, as well as the effect of air circulation in surface crevasses, is likely...

Todd, J.; Christo?ersen, P.

2014-07-02T23:59:59.000Z

150

Effect of the potential melting of the Greenland Ice Sheet on the Meridional Overturning Circulation and global climate in the future  

E-Print Network (OSTI)

., Boulder, CO 80305, USA b Department of Atmospheric and Oceanic Sciences, University of Colorado, Boulder than 3 m. This means a huge amount of freshwater will flood into the North Atlantic, which potentially

Han, Weiqing

151

U-PB SHRIMP ZIRCON AND TITANITE AGE CONSTRAINTS ON DEFORMATION ASSOCIATED WITH THE STORSTRMMEN SHEAR ZONE, NORTH-EAST GREENLAND  

E-Print Network (OSTI)

U-PB SHRIMP ZIRCON AND TITANITE AGE CONSTRAINTS ON DEFORMATION ASSOCIATED WITH THE STORSTR?MMEN with a major in Geology and titled "U-Pb SHRIMP zircon and titanite age constraints on deformation associated (sensitive, high- resolution ion-microprobe) analyses of zircon and titanite from a suite of rocks ranging

Spear, Frank S.

152

Abstract : 148 words Text : 1654 words Tables : 3 References : 29 Pages: 12  

E-Print Network (OSTI)

of the +874 T/A IFN gamma polymorphism with infections in sickle cell disease Joannes MO1 , Loko G2 roger.chout@chu-guadeloupe.fr Keywords: sickle cell, infection, polymorphism, genetic association, cytokine Abbreviated title: IFN gamma polymorphism and sickle cell disease hal-00387081,version1-23May2009

Boyer, Edmond

153

Severe proliferative retinopathy is associated with blood hyperviscosity in sickle cell hemoglobin-C disease but not in sickle cell anemia  

E-Print Network (OSTI)

Severe proliferative retinopathy is associated with blood hyperviscosity in sickle cell hemoglobin-C disease but not in sickle cell anemia Clément Lemaire1 , Yann Lamarre2 , Nathalie Lemonne3 , Xavier Waltz2, Pointe à Pitre, Guadeloupe, France. Running title: Sickle cell disease and retinopathy Corresponding

Paris-Sud XI, Université de

154

Does increased red blood cell deformability raise the risk for osteonecrosis in sickle cell Nathalie Lemonne1  

E-Print Network (OSTI)

1 Does increased red blood cell deformability raise the risk for osteonecrosis in sickle cell Pointe-à-Pitre, 97157 Pointe-à-Pitre, Guadeloupe Running head: Avascular necrosis and sickle cell anemia in sickle cell anemia (SCA) remains unknown. Blood hyper-viscosity has been suggested as a factor involved

Paris-Sud XI, Université de

155

Decreased Hematocrit-To-Viscosity Ratio and Increased Lactate Dehydrogenase Level in Patients with Sickle Cell  

E-Print Network (OSTI)

with Sickle Cell Anemia and Recurrent Leg Ulcers Philippe Connes1,2,3* , Yann Lamarre1,2 , Marie-à-Pitre, Guadeloupe Abstract Leg ulcer is a disabling complication in patients with sickle cell anemia (SCA Dehydrogenase Level in Patients with Sickle Cell Anemia and Recurrent Leg Ulcers. PLoS ONE 8(11): e79680. doi:10

Paris-Sud XI, Université de

156

Hemorheological risk factors of acute chest syndrome and painful vaso-occlusive crisis in children with sickle cell disease  

E-Print Network (OSTI)

in children with sickle cell disease Yann Lamarre1 , Marc Romana1 , Xavier Waltz1 , Marie-Laure Lalanne Guadeloupe Running title: Blood rheology in sickle cell disease Corresponding author: Philippe Connes, Ph and painful vaso-occlusive crises in children with sickle cell anemia and hemoglobin SC disease. Design

Boyer, Edmond

157

IRD/T. Jaffr IRD/M.Dukhan  

E-Print Network (OSTI)

GUYANE ArgentineArgentine Gabon Zimbawe Sri LankaSri Lanka BR?SIL ColombieColombie Togo Inde SyrieSyrie Gabon Togo ?thiopie Guadeloupe Zimbawe L'IRD DANS LE MONDE #12;RAPPORT D'ACTIVIT? ?DITORIAL 2004, date

158

Solar Activity Index: Validity Supported by Oxygen Isotope Dating  

Science Journals Connector (OSTI)

...CENTURIES OF CLIMATIC RECORD FROM CAMP CENTURY ON GREENLAND ICE SHEET, SCIENCE...sup> concentration in Greenland Camp Century ice core, correlation with solar...activity absolute age Arctic region Camp Century ice core dates general listing...

J. R. Bray

1970-05-01T23:59:59.000Z

159

Beans for Valdivia  

Science Journals Connector (OSTI)

...Antarctica (2164 m) (3, 4); from Camp Century, Greenland (1387 m) (5, 6...analysis procedure (10). The Camp Century core particles are composed primarily...Antarctica, and 1211 for the core from Camp Century, Greenland. Whether this temporal...

JONATHAN E. DAMP; DEBORAH M. PEARSALL; LAWRENCE T. KAPLAN

1981-05-15T23:59:59.000Z

160

Thermal Convection in Polar Ice Sheets Related to the Various Empirical Flow Laws of Ice  

Science Journals Connector (OSTI)

......measured and theoretical temperature profiles of the Camp Century, Greenland, borehole, J. geophys. Res., 73...measured and theoretical temperature profiles of the Camp Century, Greenland, borehole, J. geophys. Res., 73......

T. Hughes

1972-05-01T23:59:59.000Z

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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

Synchronized TerrestrialAtmospheric Deglacial Records Around the North Atlantic  

Science Journals Connector (OSTI)

...displayed (or even more pronounced) in the Dye 3, Camp Century, Renland, and Greenland Ice Sheet Project 2 (GISP2...displayed (or even more pronounced) in the Dye 3, Camp Century, Renland, and Greenland Ice Sheet Project 2 (GISP2...

Svante Bjrck; Bernd Kromer; Sigfus Johnsen; Ole Bennike; Dan Hammarlund; Geoffrey Lemdahl; Gran Possnert; Tine Lander Rasmussen; Barbara Wohlfarth; Claus Uffe Hammer; Marco Spurk

1996-11-15T23:59:59.000Z

162

Coal burning leaves toxic heavy metal legacy in the Arctic  

Science Journals Connector (OSTI)

...Cap in northeastern Canada have been reported (8). Pb is the most extensively studied, with results reported from Camp Century in northwestern Greenland (12) and Summit in central Greenland (11, 1316). A total of 36 discrete ice core...

Joseph R. McConnell; Ross Edwards

2008-01-01T23:59:59.000Z

163

Classical versus quantum coherence  

Science Journals Connector (OSTI)

...M. Stoneham Classical versus quantum coherence P. T. Greenland Department of Physics...nanostructures| Classical versus quantum coherence. | Quantum dots are structures engineered...2002.1134 Classical versus quantum coherence By P. T. Greenland Department of Physics...

2003-01-01T23:59:59.000Z

164

Pilot Program for Climate Resilience (PPCR) | Open Energy Information  

Open Energy Info (EERE)

Resilience (PPCR) Resilience (PPCR) Jump to: navigation, search Name Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Bangladesh, Bolivia, Cambodia, Dominica, Grenada, Haiti, Jamaica, Mozambique, Nepal, Niger, Papua New Guinea, Saint Lucia, Saint Vincent and the Grenadines, Samoa, Tajikistan, Tonga, Yemen, Zambia UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea

165

Saunders, A.D., Larsen, H.C., and Wise, S.W., Jr. (Eds.), 1998 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 152  

E-Print Network (OSTI)

Greenland. These rocks were erupted between 61 and 52 Ma (Sinton and Duncan, this volume) and span the whole

166

JOURNAL OF QUATERNARY SCIENCE (2001) 16 (4) 297298 Copyright 2001 John Wiley & Sons, Ltd.  

E-Print Network (OSTI)

glacial cycle and the Holocene from ice-core records obtained from six sites in Greenland (Camp Century

Hart, Jane

167

Buoyancy-Forced Downwelling in Boundary Currents MICHAEL A. SPALL  

E-Print Network (OSTI)

, such as the Greenland­Iceland­ Norwegian (GIN) Seas, Labrador Sea, Mediterranean Sea, Adriatic Sea, and Persian Gulf

168

I>KO>OOOO2& Environmental Radioactivity  

E-Print Network (OSTI)

in the Faroes and Greenland in 1987. T c data on marine samples are reported. Dau on plutonium and americium

169

Sminaire -Groupe OSUG Neige 21 mai 2010, 14 :00  

E-Print Network (OSTI)

on the Greenland ice sheet. The calibrated data model was then used to produce a roughness mosaic of the entire of the Greenland ice sheet is controlled by ice dynamics and surface-atmosphere interactions and has been used of surface roughness over the Greenland ice sheet. Data from the Multi-angle Imaging SpectroRadiometer (MISR

Ribes, Aurélien

170

Microparticle Concentration Variations Linked with Climatic Change: Evidence from Polar Ice Cores  

Science Journals Connector (OSTI)

...and 12/1 for the core from Camp Century, Greenland. Whether this temporal...and 12/1 for the core from Camp Century, Greenland. Whether this temporal...and 12/1 for the core from Camp Century, Greenland. Whether this temporal...

L. G. THOMPSON; E. MOSLEY-THOMPSON

1981-05-15T23:59:59.000Z

171

Grant Reference Principal Investigator Research Organisation Project Title NE/J013544/1 Professor B Hubbard Aberystwyth University Extended-range optical televiewer imaging of the NEEM deep ice borehole, Greenland  

E-Print Network (OSTI)

Grant Reference Principal Investigator Research Organisation Project Title NE/J013544/1 Professor B Hubbard Aberystwyth University Extended-range optical televiewer imaging of the NEEM deep ice borehole/1 Dr A Bedford Edge Hill University Late Holocene temperature reconstruction from Hawes Water northwest

172

By simulating biogeochemical cycles, the Greenland ice sheet, and more--with reach to the lower thermosphere--this system gives the research community a flexible, state-of-the-  

E-Print Network (OSTI)

climate variability and change. THE COMMUNITY EARTH SYSTEM MODEL A Framework for Collaborative Research in the CCSM4/CESM1 (version 1.0 of the Community Earth System Model) special collection of the Journal processes must be represented before a climate model becomes an Earth system model (ESM), but typically

173

E-Print Network 3.0 - anionic alkali mineral Sample Search Results  

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

of California at Berkeley Collection: Materials Science ; Chemistry 63 Boron and boron isotope systematics in the peralkaline Ilmaussaq intrusion (South Greenland) and its granitic...

174

E-Print Network Topics: E  

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

dakota eastern north greenland eastern north pacific eastern north sea eastern oil shale eastern oil shales eastern ordos basin eastern ovarian cancer eastern overthrust belt...

175

DEPARTMENT OF EARTH LABORATOIRE DE GLACIOLOGIE AND OCEAN SCIENCES ET GEOPHYSIQUE DE L'ENVIRONNEMENT  

E-Print Network (OSTI)

-evolving stratigraphy of the Greenland Ice Sheet and use the ice core records predicted at GRIP, Dye 3 and Camp Century

Paris-Sud XI, Université de

176

Global dust model intercomparison in AeroCom phase I  

E-Print Network (OSTI)

nitrate in aerosols on Midway Island, 1981 2000: EvidenceAtoll Samoa New Zealand Midway Fanning Greenland Coastalsources. The station in Midway Island (15), in central North

2011-01-01T23:59:59.000Z

177

This Week In Petroleum Summary Printer-Friendly Version  

Annual Energy Outlook 2012 (EIA)

among eight countries - Canada, Denmark (Greenland), Finland, Iceland, Norway, Russia, Sweden, and the United States. Under current international practice, countries have...

178

E-Print Network 3.0 - atlantic springer berlin Sample Search...  

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

water... Atlantic adjacent to Greenland when the THC is strong, but is ... Source: Peltier, W. Richard - Centre for Global Change Science & Department of Physics, University of...

179

1  

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

for Greenland in the future, but its impact on ice sheet flux and associated sea level rise is uncertain: direct observations of the subglacial drainage system are lacking...

180

E-Print Network 3.0 - aureus hos mennesker Sample Search Results  

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

at kunderne oplever for Summary: syge af at spise produkterne. Hos Royal Greenland Seafood AS har et sam arbejde med Danmarks Fiskeriun... for vkst af bakterier i...

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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

E-Print Network 3.0 - antarctica glacier etude Sample Search...  

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

& Geosciences 33 (2007) 104125 Remote sensing and GIS technology in the Global Land Ice Summary: (excluding Greenland and Antarctica), and thereby produce high-accuracy...

182

E-Print Network 3.0 - atlantic halibut larvae Sample Search Results  

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

larvae, Greenland halibut, newly... in the Atlantic Ocean (Bailey et al., 2005). In the Pacific Ocean, ... Source: National Oceanic and Atmospheric Administration, Pacific Marine...

183

News and Views  

Science Journals Connector (OSTI)

... It is also announced that the Danish Government steamer Oodthaab, in command of Com. Riis-Cartensen, will be conducting oceanographical work this summer in West Greenland waters.

1928-07-14T23:59:59.000Z

184

URANIUM IN ALKALINE ROCKS  

E-Print Network (OSTI)

Greenland," in Uranium Exploration Geology, Int. AtomicOklahoma," 1977 Nure Geology Uranium Symposium, Igneous HostMcNeil, M. , 1977. "Geology of Brazil's Uranium and Thorium

Murphy, M.

2011-01-01T23:59:59.000Z

185

Regional Implementation Plan for CARICOM's Climate Change Resilience  

Open Energy Info (EERE)

Jump to: navigation, search Jump to: navigation, search Name Regional Implementation Plan for CARICOM's Climate Change Resilience Framework Agency/Company /Organization Climate and Development Knowledge Network (CDKN), United Kingdom Department for International Development, Caribbean Community Climate Change Centre (CCCCC) Partner Caribbean Community Climate Change Centre (CCCCC), Caribbean Community Heads of State (CARICOM) Sector Climate, Energy, Land Topics Background analysis, Low emission development planning, Market analysis, Pathways analysis Website http://cdkn.org/project/planni Program Start 2009 Program End 2015 Country Antigua and Barbuda, Bahamas, Barbados, Belize, Dominica, Grenada, Guyana, Haiti, Jamaica, Montserrat, Saint Lucia, Saint Vincent and the Grenadines, St. Kitts and Nevis, Suriname, Trinidad and Tobago

186

Caribbean Sustainable Energy Program | Open Energy Information  

Open Energy Info (EERE)

Caribbean Sustainable Energy Program Caribbean Sustainable Energy Program Agency/Company /Organization Organization of American States (OAS) Sector Energy Focus Area Energy Efficiency, Renewable Energy Topics Market analysis, Policies/deployment programs Country St. Lucia, Dominica, Grenada, St. Kitts & Nevis, St. Vincent and the Grenadines, Antigua and Barbuda, Bahamas, Barbados UN Region Latin America and the Caribbean References OAS Project Database[1] The objective of this program is to "Facilitate the adoption of energy policies and legislation in the seven Project Countries pertaining to address the market conditions for the development and use of renewable energy and energy efficiency systems by mitigating the barriers to their use." References ↑ "OAS Project Database"

187

High-resolution record of Northern Hemisphere climate extending into the  

E-Print Network (OSTI)

of three criteria that, when satisfied together, should produce dateable ice older than that found North Greenland Ice Core Project members* *A full list of authors appears at the end of this paper ........................................................................................................................................................................................................................... Two deep ice cores from central Greenland, drilled in the 1990s, have played a key role in climate

Chappellaz, Jérôme

188

Global and Planetary Change. 7 (1993) 145-156 145 Elsevier Soence Pubhshers B V, Amsterdam  

E-Print Network (OSTI)

Camp Century, Greenland, Dunde and Guhya Ice Caps, China, Gregonev Ice Cap, Kirghxzia (formerly part reserved #12;146 L G THOMPSON ET AL Camp Century~ Fig 1 Location of the Camp Century, Greenland, Dunde and subtropics For the Dunde Ice Cap, where a long paleochmanc record is available, the warming m this century

Howat, Ian M.

189

Fabrics in Polar Ice Sheets: Development and Prediction  

Science Journals Connector (OSTI)

...Dome C (15) and Byrd Station (9), Antarctica, and Camp Century (16) and Dye 3 (17, 18), Green-land, and other...stresses characterize the base ofthe Greenland ice sheet at Camp Century and Dye 3, but temperatures are less than-13 C and...

RICHARD B. ALLEY

1988-04-22T23:59:59.000Z

190

Antarctic Ice Sheet: Stable Isotope Analyses of Byrd Station Cores and Interhemispheric Climatic Implications  

Science Journals Connector (OSTI)

...221) from the deep core hole at Camp Century in Greenland. Caution is in order...derived from deep ice cores at Camp Century in Greenland (10) displays a...Byrd Station curve, although the Camp Century curve is more detailed because...

Samuel Epstein; R. P. Sharp; A. J. Gow

1970-06-26T23:59:59.000Z

191

Photosynthetic Organism Sequenced * Environment Award Honors the Big Chill * Hands-Off Science in Higher Ed * Anthropologist Exonerated * Nature v. Culture: A Lesson From the Guppy * Nobelist Charged With Child Sex Abuse  

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...ofthe world, in the ice of Greenland and Antarctica. In the 1960s, one of the first deep ice cores was drilled at Camp Century, a U.S. military outpost in northwest Greenland, giving Dansgaard a chance to prove his theory that a 100,000-year...

1996-04-12T23:59:59.000Z

192

Early modern human settlement of Europe north of the Alps occurred 43,500 years ago in a cold steppe-type environment  

Science Journals Connector (OSTI)

...palaeotemperature records from six Greenland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland and NorthGRIP . J Quaternary...palaeotemperature records from six Greenland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland and NorthGRIP. Journal...

Philip R. Nigst; Paul Haesaerts; Freddy Damblon; Christa Frank-Fellner; Carolina Mallol; Bence Viola; Michael Gtzinger; Laura Niven; Gerhard Trnka; Jean-Jacques Hublin

2014-01-01T23:59:59.000Z

193

Radionuclide Concentrations in Surface Air: Direct Relationship to Global Fallout  

Science Journals Connector (OSTI)

...Centuries of Climatic Record from Camp Century on the Greenland Ice Sheet Abstract...the entire Greenland ice sheet at Camp Century (6). Certain physical and chemical...stable isotope dating method on the Camp Century core (see 10). The appr-oximiiate...

Michael T. Kleinman; Herbert L. Volchok

1969-10-17T23:59:59.000Z

194

Radiation Effects and Oxygen Vacancies in Silicates  

Science Journals Connector (OSTI)

...Dansgaard et al. in the Greenland Camp Century ice core (1, fig. 2) is strikingly...correlation between 1`xo in the Camp Century core and solar activity may be...con-centration in the Greenland Camp Century ice core. Century Solar 6180...

A. Chatelain; J. L. Kolopus; R. A. Weeks

1970-05-01T23:59:59.000Z

195

Dredged Trachyte and Basalt from Kodiak Seamount and the Adjacent Aleutian Trench, Alaska  

Science Journals Connector (OSTI)

...climatic changes. This is suggested by a direct comparison, cov-ering nearly 100 years, between 8 of snow strata at Camp Century on the Greenland ice sheet and measured mean air tempera-tures at Upernavik on the West Greenland coast. 16. W...

Robert B. Forbes; Charles M. Hoskin

1969-10-24T23:59:59.000Z

196

Crystal versus solution structures of enzymes: NMR spectroscopy of a crystalline serine protease  

Science Journals Connector (OSTI)

...similar origin for the basal ice in the ice cores from Camp Century (CC) and Dye-3 (D3) (Fig. 1) has been cursorily...bottom of ice cores from the Canadian Arctic Islands and Camp Century and Dye-3 in Greenland suggests that the Greenland...

SO Smith; S Farr-Jones; RG Griffin; WW Bachovchin

1989-05-26T23:59:59.000Z

197

to damage the ozone layer in the stratosphere and are banned in developed countries. They are used as refrigerants, propellants,  

E-Print Network (OSTI)

hexafluoride (SF6 ), GWP: 23,900 This is produced for use as an insulator in various kinds of elec- trical/navigating-the-numbers (accessed May 31, 2008). --DAVID J. CUFF GREENLAND ICE SHEET The Greenland ice sheet is the second largest ice mass on Earth and is about one-tenth the volume of the Antarctic ice sheet. It is the only

Huybrechts, Philippe

198

1302 VOLUME 16J O U R N A L O F C L I M A T E 2003 American Meteorological Society  

E-Print Network (OSTI)

of Greenland Ice Sheet Surface Climate in the HIRHAM Regional Climate Model Using Automatic Weather Station Data JASON E. BOX Byrd Polar Research Center, The Ohio State University, Columbus, Ohio ANNETTE RINKE of Greenland ice sheet surface climate are made with the 0.5 -horizontal resolution HIRHAM regional climate

Box, Jason E.

199

Northern Paths to Aboriginal Self-Determination  

E-Print Network (OSTI)

are at the forefront of solutions to accommodate the divide between these communities. Aboriginal peoples seek-determination. Since 1380, the Inuit of Greenland have been under Danish rule, and formally Greenland was a colony. The Sami Parliament, however, only has advisory powers to the Norwegian Storting (legislature) and does

Northern British Columbia, University of

200

Black carbon in Arctic snow and its effect on surface albedo  

E-Print Network (OSTI)

= 1000 µm Typical values of BC in Arctic snow (ppb): Greenland 2-3 Canada 10 Siberia 20-25 #12 = 1000 µm Typical values of BC in Arctic snow (ppb): Greenland 2-3 Canada 10 Siberia 20-25 Snow grain large areas of snow are exposed to significant solar energy (snow albedo is less important in winter

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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.


201

Recent Metal Pollution in Agassiz Ice Cap  

Science Journals Connector (OSTI)

This is probably due to the close proximity and similar elevation of the two areas (Agassiz Ice Cap, Canadian Arctic and Camp Century, northwest Greenland), which are likely subjected to the same polluted air masses. ... Figure 3 shows Pb concentrations covering the past 250 years for three different Arctic areas:? Camp Century, northwest Greenland (dashed line, ref 1); Summit, central Greenland (solid line, ref 8); and Agassiz Ice Cap (star symbols, this work). ... Since Camp Century is lower than Summit (1866 vs 3228 m above sea level) and is expected to receive more pollution, the relative position of the two lines is reasonable, the dashed line being higher than the solid one. ...

V. Cheam; G. Lawson; J. Lechner; R. Desrosiers

1998-11-10T23:59:59.000Z

202

Neanderthal extinction by competitive exclusion  

E-Print Network (OSTI)

-latitude North Atlantic sea surface temperatures had marked rapid impacts on continental climate and vegetation. Greenland Interstadials (GI; mild phases) were characterized in Western Europe by open forest landscapes, while herbaceous-dominated landscapes... not extinction) occurred: Greenland Interstadials 911 (pre-H4; 43.3 40.2 kyr cal BP, see [48]), Heinrich event 4 (H4; 40.238.6 kyr cal BP), and Greenland Interstadial 8 (GI8; 38.636.5 kyr cal BP). GI911 were three short-term mild events separated by two...

Banks, William E.; d'Errico, Francesco; Peterson, A. Townsend; Kageyama, Masa; Sima, Adriana; Sanchez-Goni, Maria-Fernanda

2008-12-24T23:59:59.000Z

203

1  

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

Meltwater effects on flow of Greenland's Meltwater effects on flow of Greenland's ice sheet less severe for sea level rise than earlier feared, scientists say August 19, 2013 LOS ALAMOS, N.M., Aug. 19, 2013-The effects of increased melting on the future motion of and sea-level contribution from Greenland's massive ice sheet are not quite as dire as previously thought, according to a new study from an international team of researchers. In a paper published this month in Proceedings of the National Academy of Sciences (PNAS), the team found that accelerating ice sheet movement from increasing meltwater lubrication is likely to have only a minor role in future sea-level rise, when compared with other factors like increased iceberg production and surface melting. Greenland's ice sheet is the world's second largest body of ice. A melt event impacting

204

29  

Science Journals Connector (OSTI)

Apr 27, 1983 ... during thermonuclear tests in the late 1950s and early 1960s. By comparison, in 1972 surficial waters in the Greenland Sea showed a value of...

2000-02-09T23:59:59.000Z

205

LMS-AMC-S01980-0-0.cdr  

Office of Legacy Management (LM)

tons) in the Bering Sea and Aleutian Islands, 1965-2005 Year Pollock Pacific Cod Sable Fish Yellow Fin Sole Greenland Turbot Arrow Tooth Flounder a Rock Sole c Other Flat Fish...

206

Anthropogenic lead dynamics in the terrestrial and marine environment  

Science Journals Connector (OSTI)

...shown in gure 7, re ect the introduction and phase-out of leaded petrol. Measuring lead concentrations in ice near Camp Century, Greenland, Murozumi et al. (1969) rst observed the Arctic anthropogenic transient, with lead concentrations increas...

2002-01-01T23:59:59.000Z

207

Simulating Arctic Climate Warmth and Icefield Retreat in the  

E-Print Network (OSTI)

, Devon, and Meighen ice caps in the Canadian Arctic, and possibly in Camp Century (northwest Greenland- atures markedly warmer than those in the 20th century and the late Holocene, and it also featured

Ingólfsson, ?lafur

208

Ice Cores and Climatic Change  

Science Journals Connector (OSTI)

...from Vostok and Byrd stations in Antarctica and from Camp Century in Greenland. Vostok is the simplest case glaciologically, Camp Century the most complex. On purely glaciological grounds it...

1977-01-01T23:59:59.000Z

209

Facing future climate change: is the past relevant?  

Science Journals Connector (OSTI)

...less so. Since the nineteenth century, it has been suspected that both...which occurred over several centuries and were linked to regional temperature...Greenland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland...

2008-01-01T23:59:59.000Z

210

SCIENTIFIC PROGRAM AND ABSTRACTS OF CONTRIBUTED PAPERS  

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...provided continuous cores from the surface com- pletely through vertical profiles of both the Greenland ice sheet at Camp Century (1375 m) and the Antarctic ice sheet at Byrd Station (2164 m). A comprehensive and detailed core study program...

1969-01-01T23:59:59.000Z

211

A Perspective on Climatic Change  

Science Journals Connector (OSTI)

...VARIATIONS ON CLIMATE OF EARTH, TELLUS 21 : 611 ( 1969 ). DANSGAARD, W, ONE THOUSAND CENTURIES OF CLIMATIC RECORD FROM CAMP CENTURY ON GREENLAND ICE SHEET, SCIENCE 166 : 377 ( 1969 ). DAVITAYA, F.F., ATMOSPHERIC DUST CONTENT AS A FACTOR AFFECTING...

Reid A. Bryson

1974-05-17T23:59:59.000Z

212

Pfaudler-Permutit Plans Hot Waste Treater  

Science Journals Connector (OSTI)

One is already in operation at Camp Century, Greenlandthe PM- 2A (portable medium power plant) which the Corps of Engineers calls a research and development reactor. ...

1961-01-09T23:59:59.000Z

213

Climatic Ice Core Records from the Tropical Quelccaya Ice Cap  

Science Journals Connector (OSTI)

...DANSGAARD, W, LATE CENOZOIC GLACIA 37 ( 1971 ). DANSGAARD, W, ONE THOUSAND CENTURIES OF CLIMATIC RECORD FROM CAMP CENTURY ON GREENLAND ICE SHEET, SCIENCE 166 : 377 ( 1969 ). DANSGAARD, W, STABLE ISOTOPES IN PRECIPITATION, TELLUS 16...

LONNIE G. THOMPSON; STEFAN HASTENRATH; BENJAMN MORALES ARNAO

1979-03-23T23:59:59.000Z

214

Deuterium Content of Peat as a Paleoclimatic Recorder  

Science Journals Connector (OSTI)

...Netherlands. CRAIG, H, SCIENCE 133 : 3467 ( 1961 ). DANSGAARD, W, ONE THOUSAND CENTURIES OF CLIMATIC RECORD FROM CAMP CENTURY ON GREENLAND ICE SHEET, SCIENCE 166 : 377 ( 1969 ). DANSGAARD, W, STABLE ISOTOPES IN PRECIPITATION, TELLUS 16...

W. E. Schiegl

1972-02-04T23:59:59.000Z

215

Iceberg discharges of the last glacial period driven by oceanic circulation changes  

Science Journals Connector (OSTI)

...1522 . 42 Johnsen SJ ( 2001 ) Oxygen isotope and palaeotemperature records from six Greenland ice-core stations: Camp century, dye-3, grip, gisp2, renland and northgrip . J Quat Sci 16 : 299 307 . We thank A. Ganopolski for helpful...

Jorge Alvarez-Solas; Alexander Robinson; Marisa Montoya; Catherine Ritz

2013-01-01T23:59:59.000Z

216

Late Glacial Stage and Holocene Tropical Ice Core Records from Huascarn, Peru  

Science Journals Connector (OSTI)

...INSOLUBLE IMPURITY PROFILES FROM THE DEVON ISLAND AND CAMP CENTURY ICE CORES, QUATERNARY RESEARCH 11 : 299 ( 1979...Byrd Station (7) and Vostok (12) in Ant-arctica, Camp Century (7) and Summit (10) in Greenland, Devon Island...

L. G. Thompson; E. Mosley-Thompson; M. E. Davis; P. -N. Lin; K. A. Henderson; J. Cole-Dai; J. F. Bolzan; K. -b. Liu

1995-07-07T23:59:59.000Z

217

Isotopic Composition of Atmospheric Moisture  

Science Journals Connector (OSTI)

Similar results were obtained by Dansgaard et al. (1969) for 1,300m ice column from a borehole at Camp Century Station in Greenland and also by Gordienko and Kotlyakov (1976) while studying an ice column 1,00...

V. I. Ferronsky; V. A. Polyakov

2012-01-01T23:59:59.000Z

218

New evidence for enhanced cosmogenic isotope production rate in the atmosphere 37 ka BP  

E-Print Network (OSTI)

and others, 1987; Kocharov, 1990). Records of 10 Be in the Byrd (West Antarctica) ice core and in the Camp Century (Greenland) ice core further aroused inter- est in the possibility of using10 Be as atime marker

Howat, Ian M.

219

Pleistocene Paleotemperatures  

Science Journals Connector (OSTI)

...DAMUTH, J.E., B GEOL SOC AM 81 : 189 ( 1970 ). DANSGAARD, W, ONE THOUSAND CENTURIES OF CLIMATIC RECORD FROM CAMP CENTURY ON GREENLAND ICE SHEET, SCIENCE 166 : 377 ( 1969 ). DANSGAARD, W, GLACIER OXYGEN-18 CONTENT AND PLEISTOCENE OCEAN...

C. Emiliani

1970-05-15T23:59:59.000Z

220

Global climate evolution during the last deglaciation  

Science Journals Connector (OSTI)

...26423 . 151 Johnsen SJ ( 2001 ) Oxygen isotope and palaeotemperature records from six Greenland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland and NorthGRIP...

Peter U. Clark; Jeremy D. Shakun; Paul A. Baker; Patrick J. Bartlein; Simon Brewer; Ed Brook; Anders E. Carlson; Hai Cheng; Darrell S. Kaufman; Zhengyu Liu; Thomas M. Marchitto; Alan C. Mix; Carrie Morrill; Bette L. Otto-Bliesner; Katharina Pahnke; James M. Russell; Cathy Whitlock; Jess F. Adkins; Jessica L. Blois; Jorie Clark; Steven M. Colman; William B. Curry; Ben P. Flower; Feng He; Thomas C. Johnson; Jean Lynch-Stieglitz; Vera Markgraf; Jerry McManus; Jerry X. Mitrovica; Patricio I. Moreno; John W. Williams

2012-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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.


221

Ris-M-2914 List ofSelected Publications  

E-Print Network (OSTI)

at Thule, Greenland in 1968 - The risk assessment calculations on the Swedish Barseback power plant and technical papers written by staff members of the former Health Physics Department of Risø National

222

Pre-Columbian origins of Native American dog breeds, with only limited replacement by European dogs, confirmed by mtDNA analysis  

Science Journals Connector (OSTI)

...and Greenland dogs, Alaskan Malamute, Chihuahua, xoloitzcuintli and perro sin pelo del...unique haplotype between the Mexican breed Chihuahua and ancient Mexican samples. We also...continent, for example, the Mexican Chihuahua, the xoloitzcuintli (Mexican hairless...

2013-01-01T23:59:59.000Z

223

Integration of a 15-Element, VHF Bow-Tie Antenna Array into an Aerodynamic Fairing on a NASA P-3 Aircraft  

E-Print Network (OSTI)

Radar depth sounding and imaging of deep glaciers in Antarctica and Greenland yield results for better understanding a changing climate and improving glacier modeling. A 15-element, airborne antenna array with an increased ...

Byers, Kyle J.

2011-06-16T23:59:59.000Z

224

Download Full-text PDF  

Science Journals Connector (OSTI)

in permanently cold (from 1.7C to 4C) sediments off the east and west coasts of Greenland. The investigated ...... In B. Bolin and R. B. Cook [eds.], The major.

2004-08-17T23:59:59.000Z

225

Multi-parameter estimation in glacier models with adjoint and algorithmic differentiation  

E-Print Network (OSTI)

The cryosphere is comprised of about 33 million km of ice, which corresponds to 70 meters of global mean sea level equivalent [30]. Simulating continental ice masses, such as the Antarctic or Greenland Ice Sheets, requires ...

Davis, Andrew D. (Andrew Donaldson)

2012-01-01T23:59:59.000Z

226

A Reconciled Estimate of Ice-Sheet Mass Balance  

Science Journals Connector (OSTI)

...Reassessment of net surface mass balance in Antarctica...high-resolution surface mass balance map of Antarctica (1979-2010...from ice-sheet-wide velocity mapping . J. Glaciol...J. ., Higher surface mass balance of the Greenland...

Andrew Shepherd; Erik R. Ivins; Geruo A; Valentina R. Barletta; Mike J. Bentley; Srinivas Bettadpur; Kate H. Briggs; David H. Bromwich; Ren Forsberg; Natalia Galin; Martin Horwath; Stan Jacobs; Ian Joughin; Matt A. King; Jan T. M. Lenaerts; Jilu Li; Stefan R. M. Ligtenberg; Adrian Luckman; Scott B. Luthcke; Malcolm McMillan; Rakia Meister; Glenn Milne; Jeremie Mouginot; Alan Muir; Julien P. Nicolas; John Paden; Antony J. Payne; Hamish Pritchard; Eric Rignot; Helmut Rott; Louise Sandberg Srensen; Ted A. Scambos; Bernd Scheuchl; Ernst J. O. Schrama; Ben Smith; Aud V. Sundal; Jan H. van Angelen; Willem J. van de Berg; Michiel R. van den Broeke; David G. Vaughan; Isabella Velicogna; John Wahr; Pippa L. Whitehouse; Duncan J. Wingham; Donghui Yi; Duncan Young; H. Jay Zwally

2012-11-30T23:59:59.000Z

227

Seasonal Mixing Processes in an Arctic Fjord System  

Science Journals Connector (OSTI)

Studies of water movement in the Aafardlikavs/Qaumarujuk fjord system in West Greenland have barn carried out in order to understand the movement of mine tailings discharged into Agfardlikavs Fjord. Observations are explained in terms of ...

E. L. Lewis; R. G. Perkin

1982-01-01T23:59:59.000Z

228

Correction of ADCP compass errors resulting from iron in the instruments vicinity  

Science Journals Connector (OSTI)

Iron in the vicinity of compasses results in compass deviations. ADCPs mounted on steel buoyancy devices and deployed on seven moorings on the East Greenland outer shelf and upper slope from 2007 to 2008 suffered from severe compass deviations as ...

Wilken-Jon von Appen

229

Climate Change, Windows, Lighting, and Cooling  

Science Journals Connector (OSTI)

The recent findings on temperature variability in Greenland for the last 150,000 years are discussed and related to the threat of greenhouse warming from CO2. Then we describe three cost-effective technologies fo...

A. H. Rosenfeld

1994-01-01T23:59:59.000Z

230

1  

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

Meltwater effects on flow of Greenland's ice sheet less severe for sea level rise than earlier feared, scientists say August 19, 2013 LOS ALAMOS, N.M., Aug. 19, 2013-The effects of...

231

1663  

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

inside busy computer networks Spotlights Moulin bleu A rare morsel of good news about sea-level rise from the Greenland ice sheet How to spot a nuke Laser-driven blast of neutrons...

232

News Stories  

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

Scientific Computing Greenland Ice Sheet "Sliding" a Small Contributor to Future Sea-Level Rise Awards LANL FES PI selected as Fellow by the APS Division of Plasmas Physics...

233

Energy content and fecundity of capelin (Mallotus villosus) along a 1,500-km latitudinal gradient  

Science Journals Connector (OSTI)

Capelin is a planktivorous key fish species in many subarctic ecosystems representing the link between lower trophic levels and apex predators. Little is known, however, of capelin in Greenland waters, but it has...

R. Hedeholm; P. Grnkjr; S. Rysgaard

2011-06-01T23:59:59.000Z

234

E-Print Network 3.0 - albedo flat map Sample Search Results  

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

to Infer Snow Albedo From the Summary: . For example, Fig. 1. Map of the Greenland ice sheet showing the AWS locations used for the albedo comparisons... to Infer Snow Albedo...

235

E-Print Network 3.0 - atlantic halibut hippoglossus Sample Search...  

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

early life stages in the Summary: in the Atlantic Ocean (Bailey et al., 2005). In the Pacific Ocean, Greenland halibut is pri- marily found... . In the Atlantic, Stene et al....

236

A normative model of peer review: qualitative assessment of manuscript reviewers attitudes towards peer review  

E-Print Network (OSTI)

my own skills Course on peer review skills Special rates forR, Simon G. Chance and consensus in peer review. Science.Emanuel L, Greenland P. Peer Review and Professionalism at

Tercier, John; Callaham, Michael L.

2007-01-01T23:59:59.000Z

237

Circulation and convection in the Irminger Sea  

E-Print Network (OSTI)

Aspects of the circulation and convection in the Irminger Sea are investigated using a variety of in-situ, satellite, and atmospheric reanalysis products. Westerly Greenland tip jet events are intense, small-scale wind ...

Vge, Kjetil

2010-01-01T23:59:59.000Z

238

NERSC Supercomputers Help Explain the Last Big Freeze  

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

transported it to the North Atlantic (near Greenland), allowing it to disrupt the ocean's heat engine. "With 18 kilometers between each grid-point, we have the highest resolution...

239

Oceanic Boundary Conditions for Jakobshavn Glacier: Part I. Variability and Renewal of Ilulissat Icefjord Waters, 2001-2014  

Science Journals Connector (OSTI)

Jakobshavn Glacier, West Greenland, has responded to temperature changes in Ilulissat Icefjord, into which it terminates. We collected hydrographic observations inside this silled fjord and from adjacent Disko Bay between 2001 and 2014. The ...

Carl V. Gladish; David M. Holland; Aqqalu Rosing-Asvid; Jane W. Behrens; Jesper Boje

240

Download  

Science Journals Connector (OSTI)

Apr 27, 1983 ... during thermonuclear tests in the late 1950s and early 1960s. By comparison, in 1972 surficial waters in the Greenland Sea showed a value of...

2000-02-09T23:59:59.000Z

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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.


241

Oxygen isotope anomaly observed in water vapor from Alert, Canada and the implication for the stratosphere  

Science Journals Connector (OSTI)

...stratospheric input of anomalous water, injections of stratospheric tritium (mainly produced by atmospheric detonations of thermonuclear devices during 1954?1963) to various sites in Greenland and Antarctica were recorded in snow pits (e.g., ref...

Ying Lin; Robert N. Clayton; Lin Huang; Noboru Nakamura; James R. Lyons

2013-01-01T23:59:59.000Z

242

Caribbean Community (CARICOM) Sustainable Energy Roadmap and Strategy |  

Open Energy Info (EERE)

Caribbean Community (CARICOM) Sustainable Energy Roadmap and Strategy Caribbean Community (CARICOM) Sustainable Energy Roadmap and Strategy Jump to: navigation, search Name Caribbean Community (CARICOM) Sustainable Energy Roadmap and Strategy Agency/Company /Organization Inter-American Development Bank, World Watch Institute (WWI) Sector Climate, Energy Focus Area Renewable Energy, Economic Development, Energy Efficiency, Greenhouse Gas, Grid Assessment and Integration, Industry, People and Policy, Transportation Topics Background analysis, Baseline projection, Finance, GHG inventory, Implementation, Low emission development planning, -Roadmap, Market analysis, Policies/deployment programs, Resource assessment, Technology characterizations Program Start 2012 Program End 2012 Country Antigua and Barbuda, Bahamas, Barbados, Belize, Dominica, Grenada, Guyana, Haiti, Jamaica, Montserrat, St. Lucia, St. Vincent and the Grenadines, St. Kitts and Nevis, Suriname, Trinidad and Tobago

243

Energy-Economic Information System (SIEE) | Open Energy Information  

Open Energy Info (EERE)

Energy-Economic Information System (SIEE) Energy-Economic Information System (SIEE) Jump to: navigation, search Tool Summary LAUNCH TOOL Name: Energy-Economic Information System (SIEE) Database Agency/Company /Organization: Latin American Energy Organization Sector: Energy Topics: Baseline projection, GHG inventory, Background analysis Resource Type: Dataset Website: www.olade.org/sieeEn.html Country: Costa Rica, El Salvador, Guatemala, Honduras, Nicaragua, Panama, Mexico, Argentina, Bolivia, Brazil, Chile, Colombia, Ecuador, Guyana, Paraguay, Peru, Suriname, Uruguay, Venezuela, Barbados, Cuba, Grenada, Haiti, Jamaica, Trinidad & Tobago, Dominican Republic Central America, Central America, Central America, Central America, Central America, Central America, Central America, South America, South America, South America, South America, South America, South America, South America, South America, South America, South America, South America, South America, Caribbean, Caribbean, Caribbean, Caribbean, Caribbean, Caribbean, Caribbean

244

OLADE-Latin American and Caribbean Energy Efficiency Seminar | Open Energy  

Open Energy Info (EERE)

OLADE-Latin American and Caribbean Energy Efficiency Seminar OLADE-Latin American and Caribbean Energy Efficiency Seminar Jump to: navigation, search Tool Summary LAUNCH TOOL Name: OLADE-Latin American and Caribbean Energy Efficiency Seminar Agency/Company /Organization: Latin America Energy Organization Sector: Energy Focus Area: Energy Efficiency Topics: Implementation, Technology characterizations Resource Type: Presentation, Webinar, Workshop, Lessons learned/best practices Website: www.olade.org/eficiencia/indexEn.html Country: Costa Rica, El Salvador, Guatemala, Honduras, Nicaragua, Panama, Mexico, Argentina, Bolivia, Brazil, Chile, Colombia, Ecuador, Guyana, Paraguay, Peru, Suriname, Uruguay, Venezuela, Barbados, Cuba, Grenada, Haiti, Jamaica, Trinidad & Tobago, Dominican Republic Central America, Central America, Central America, Central America, Central America, Central America, Central America, South America, South America, South America, South America, South America, South America, South America, South America, South America, South America, South America, South America, Caribbean, Caribbean, Caribbean, Caribbean, Caribbean, Caribbean, Caribbean

245

Saint Vincent and the Grenadines-Pilot Program for Climate Resilience  

Open Energy Info (EERE)

Saint Vincent and the Grenadines-Pilot Program for Climate Resilience Saint Vincent and the Grenadines-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Saint Vincent and the Grenadines-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Saint Vincent and the Grenadines UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan

246

Step-by-Step Instructions  

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

Mississippi Mississippi based upon the simple prescriptive option of the 2012 IECC. It does not provide a guarantee for meeting the IECC. This guide is not designed to reflect the actual energy code, with amendments, if any, adopted in Mississippi and does not, therefore, provide a guarantee for meeting the state energy code. For details on the energy code adopted by Mississippi, including how it may differ from the IECC, please contact your local building code official. Additional copies of this guide are available on www.reca-codes.com. CLIMATE ZONE 3 Adams Greene Lowndes Smith Alcorn Grenada Madison Sunflower Amite Hinds Marion Tallahatchie Attala Holmes Marshall Tate Benton Humphreys Monroe Tippah Bolivar Issaquena Montgomery Tishomingo Calhoun Itawamba Neshoba Tunica

247

OLADE Sustainable Energy Planning Manual | Open Energy Information  

Open Energy Info (EERE)

OLADE Sustainable Energy Planning Manual OLADE Sustainable Energy Planning Manual Jump to: navigation, search Tool Summary Name: OLADE Sustainable Energy Planning Manual Agency/Company /Organization: Latin American Energy Organization Sector: Energy Focus Area: Energy Efficiency, Renewable Energy Topics: Implementation, Background analysis Website: www.olade.org/proyectoPlanificacionEnergetica.html Country: Costa Rica, El Salvador, Guatemala, Honduras, Nicaragua, Panama, Mexico, Argentina, Bolivia, Brazil, Chile, Colombia, Ecuador, Guyana, Paraguay, Peru, Suriname, Uruguay, Venezuela, Barbados, Cuba, Grenada, Haiti, Jamaica, Trinidad & Tobago, Dominican Republic Central America, Central America, Central America, Central America, Central America, Central America, Central America, South America, South America, South America, South America, South America, South America, South America, South America, South America, South America, South America, South America, Caribbean, Caribbean, Caribbean, Caribbean, Caribbean, Caribbean, Caribbean

248

Legal Energy Information System (SIEL) Database | Open Energy Information  

Open Energy Info (EERE)

Legal Energy Information System (SIEL) Database Legal Energy Information System (SIEL) Database Jump to: navigation, search Tool Summary Name: Legal Energy Information System (SIEL) Database Agency/Company /Organization: Latin American Energy Organization Sector: Energy Focus Area: Renewable Energy Topics: Policies/deployment programs, Background analysis Resource Type: Dataset Website: www.olade.org/sielEn.html Country: Costa Rica, El Salvador, Guatemala, Honduras, Nicaragua, Panama, Mexico, Argentina, Bolivia, Brazil, Chile, Colombia, Ecuador, Guyana, Paraguay, Peru, Suriname, Uruguay, Venezuela, Barbados, Cuba, Grenada, Haiti, Jamaica, Trinidad & Tobago, Dominican Republic Central America, Central America, Central America, Central America, Central America, Central America, Central America, South America, South America, South America, South America, South America, South America, South America, South America, South America, South America, South America, South America, Caribbean, Caribbean, Caribbean, Caribbean, Caribbean, Caribbean, Caribbean

249

Regional Implementation Plan for CARICOM's Climate Change Resilience  

Open Energy Info (EERE)

(Redirected from CDKN-CARICOM-Trinidad and Tobago-A Regional Implementation (Redirected from CDKN-CARICOM-Trinidad and Tobago-A Regional Implementation Plan for CARICOM's Regional Climate Change Resilience Framework) Jump to: navigation, search Name Regional Implementation Plan for CARICOM's Climate Change Resilience Framework Agency/Company /Organization Climate and Development Knowledge Network (CDKN), United Kingdom Department for International Development, Caribbean Community Climate Change Centre (CCCCC) Partner Caribbean Community Climate Change Centre (CCCCC), Caribbean Community Heads of State (CARICOM) Sector Climate, Energy, Land Topics Background analysis, Low emission development planning, Market analysis, Pathways analysis Website http://cdkn.org/project/planni Program Start 2009 Program End 2015 Country Antigua and Barbuda, Bahamas, Barbados, Belize, Dominica, Grenada, Guyana, Haiti, Jamaica, Montserrat, Saint Lucia, Saint Vincent and the Grenadines, St. Kitts and Nevis, Suriname, Trinidad and Tobago

250

CDKN-CARICOM-A Regional Implementation Plan for CARICOM's Regional  

Open Energy Info (EERE)

CARICOM-A Regional Implementation Plan for CARICOM's Regional CARICOM-A Regional Implementation Plan for CARICOM's Regional Climate Change Resilience Framework Jump to: navigation, search Name CDKN-CARICOM-A Regional Implementation Plan for CARICOM's Regional Climate Change Resilience Framework Agency/Company /Organization Climate and Development Knowledge Network (CDKN), United Kingdom Department for International Development Partner Caribbean Community Climate Change Centre (CCCCC), Caribbean Community Heads of State (CARICOM) Sector Climate, Energy, Land Topics Background analysis, Market analysis, Pathways analysis Website http://cdkn.org/project/planni Program Start 2010 Country Antigua and Barbuda, The Bahamas, Barbados, Belize, Dominica, Grenada, Guyana, Haiti, Jamaica, Montserrat, Saint Lucia, St. Kitts and Nevis, St. Vincent and the Grenadines, Suriname, Trinidad and Tobago

251

Papua New Guinea-Pilot Program for Climate Resilience (PPCR) | Open Energy  

Open Energy Info (EERE)

Page Page Edit with form History Facebook icon Twitter icon » Papua New Guinea-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Papau New Guinea-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Papau New Guinea UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa

252

Green Solar | Open Energy Information  

Open Energy Info (EERE)

Solar Solar Place Paris, France Zip 45003 Product Develops and builds PV systems in Guadeloupe and Mauritius. Coordinates 48.85693°, 2.3412° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":48.85693,"lon":2.3412,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

253

Bringing simulation to implementation: Presentation of a global approach in the design of passive solar buildings under humid tropical climates  

E-Print Network (OSTI)

In early 1995, a DSM pilot initiative has been launched in the French islands of Guadeloupe and Reunion through a partnership between several public and private partners (the French Public Utility EDF, the University of Reunion Island, low cost housing companies, architects, energy consultants, etc...) to set up standards to improve thermal design of new residential buildings in tropical climates. This partnership led to defining optimized bio-climatic urban planning and architectural designs featuring the use of passive cooling architectural principles (solar shading, natural ventilation) and components, as well as energy efficient systems and technologies. The design and sizing of each architectural component on internal thermal comfort in building has been assessed with a validated thermal and airflow building simulation software (CODYRUN). These technical specifications have been edited in a reference document which has been used to build over 300 new pilot dwellings through the years 1996-1998 in Reunion...

Garde, Franois; Celaire, Robert

2012-01-01T23:59:59.000Z

254

Effect of ocean temperature on southwestern U.S. climate analyzed  

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

December » December » Effect of ocean temperature on southwestern climate Effect of ocean temperature on southwestern U.S. climate analyzed Researchers concluded that only part of the recent temperature rise in the Southwest could be attributed to greenhouse gases. December 19, 2013 Image from National Oceanic and Atmospheric Administration's Environmental Visualization Laboratory depicts sea surface temperatures around Greenland from October 2010. Image from National Oceanic and Atmospheric Administration's Environmental Visualization Laboratory depicts sea surface temperatures around Greenland from October 2010. Assuming that the past is a good indicator of the future, the scientists conclude that there should be wetter times ahead. Researchers have analyzed the relationship between a natural phenomenon in

255

Seismic Travel-Time Residuals and Plates  

Science Journals Connector (OSTI)

......United States, Canada and Greenland under the auspices of Project Vela Uniform (Long Range Seismic Measurements 1966). Arrival...1 that if we plot residuals on the focal sphere, we are at liberty to ascribe these residuals to source effects, receiver effects......

D. Davies; D. P. McKenzie

1969-09-01T23:59:59.000Z

256

*Deborah E. Eason, Garrett Ito, John M. Sinton Insights into melt and chemical transport rates in the mantle  

E-Print Network (OSTI)

*Deborah E. Eason, Garrett Ito, John M. Sinton Insights into melt and chemical transport rates Greenland Ice-Core Project (NGRIP) Members (2004) Nature Sinton, J., Grönvold, K., Sæmundsson, K. (2005) G3. These data supplement existing fini- and post-glacial data [Sinton et al., 2005] to form a detailed eruptive

Geist, Dennis

257

Integrated stratigraphy of the Oligocene pelagic sequence in the Umbria-Marche basin (northeastern Apennines, Italy): A potential Global Stratotype Section and Point (GSSP) for the Rupelian/Chattian boundary  

Science Journals Connector (OSTI)

...Neri4, David M. Bice56, Henk Brinkhuis7, Nathan Church89, Alison Macalady89, Aaron McDaniel89, Alain Deino10, Fabrizio Lirer11...Greenland Margin): in Saunders, A.D., Larsen, H.C., and Wise, S.W. Jr., eds., Proceedings of the Ocean Drilling ProgramScientific...

Rodolfo Coccioni; Andrea Marsili; Alessandro Montanari; Adriana Bellanca; Rodolfo Neri; David M. Bice; Henk Brinkhuis; Nathan Church; Alison Macalady; Aaron McDaniel; Alain Deino; Fabrizio Lirer; Mario Sprovieri; Patrizia Maiorano; Simonetta Monechi; Claudio Nini; Marisa Nocchi; Jrg Pross; Pierre Rochette; Leonardo Sagnotti; Fabio Tateo; Yannick Touchard; Stefaan Van Simaeys; Graham L. Williams

258

Coupled variability and air-sea interaction in the South Atlantic Andreas Sterl, Wilco Hazeleger  

E-Print Network (OSTI)

and Tanimoto (1998) describe a pan-Atlantic SST pattern reaching from South Africa to Greenland. Most studiesCoupled variability and air-sea interaction in the South Atlantic Ocean Andreas Sterl, Wilco mechanisms involved in forcing and damping of Sea Surface Temperature (SST) variability in the South Atlantic

Haak, Hein

259

Analysis and modelling of glacial climate transitions using simple dynamical systems  

Science Journals Connector (OSTI)

...e2009-01087-5 ) 25 Johnsen, SJ , . 2001 Oxygen isotope and palaeotemperature records from six Greenland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland and NorthGRIP. J. Q. Sci. 16. 299-307. 10.1002/jqs.622 ( doi:10...

2013-01-01T23:59:59.000Z

260

Post-glacial partitioning of mitochondrial genetic variation in the field vole  

Science Journals Connector (OSTI)

...Sveinbjornsdottir, and J. White 2001 Oxygen isotope and palaeotemperature records from six Greenland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland and NorthGRIP. J. Quaternary Sci. 16, 299-307. 10.1002/jqs.622 ( doi...

2011-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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.


261

Behaviorally evoked hippocampal theta waves: a cholinergic response  

Science Journals Connector (OSTI)

...full-fledged Arctic ice cap. The first is based on the Greenland air temperature record obtained from isotopic studies of the Camp Century ice core. The second is based on the oxygen isotope record ofbenthicforaminiferafrom a deep Pacific Ocean core.

H Teitelbaum; JF Lee; JN Johannessen

1975-06-13T23:59:59.000Z

262

Glacier Oxygen-18 Content and Pleistocene Ocean Temperatures  

Science Journals Connector (OSTI)

...CENTURIES OF CLIMATIC RECORD FROM CAMP CENTURY ON GREENLAND ICE SHEET, SCIENCE...the inland ice to the bed rock at Camp Century has recently been measured (16...of the glaciated areas. In the Camp Century core this effect was measured to-12...

W. Dansgaard; Henrik Tauber

1969-10-24T23:59:59.000Z

263

AntarcticaContinent of International Science  

Science Journals Connector (OSTI)

...records are becoming available from ice cores. Deep-drilling techniques are being perfected at the U.S. Army's Camp Century in Green-land and will, in the predictable future, enable us to obtain cores through more than 10,000 feet of...

Laurence M. Gould

1965-12-31T23:59:59.000Z

264

Gravitational Separation of Gases and Isotopes in Polar Ice Caps  

Science Journals Connector (OSTI)

...reported that 02 trapped in 2000-year-old ice from Camp Century, Green-land, has an 180/160 enrichment given by...values for 02 in 6,100-and 20,000-year-old Camp Century ice (1), and noting that mean seawater was enriched...

H. Craig; Y. Horibe; T. Sowers

1988-12-23T23:59:59.000Z

265

Very Heavy Solar Cosmic Rays: Energy Spectrum and Implications for Lunar Erosion  

Science Journals Connector (OSTI)

...years in the periodicity of glacial advance (2, 3) and in the temperature-related 8180 data from the Greenland Camp Century ice core (4). There is evidence that these cycles are based on 1242 face were removed for each incident solar wind...

R. L. Fleischer; H. R. Hart JR.; G. M. Comstock

1971-03-26T23:59:59.000Z

266

Celestial Mechanics Experiment  

Science Journals Connector (OSTI)

...at-mosphere. The facilities and methods for col-lecting particulate material from 100-to 300-year-old ice at Camp Century, Greenland, have been described (5). In our work, columns containing ca-tion-exchange or mixed cationand anion-exchange...

J. D. Anderson; G. E. Pease; L. Efron; R. C. Tausworthe

1967-12-29T23:59:59.000Z

267

Neutron Activation for Distinguishing Cascade Range Pyroclastics  

Science Journals Connector (OSTI)

...unconsolidated sediment, such as glacial till, rather than solid rock. Glacial till underlies the Greenland ice sheet at Camp Century (4). Liquid water was encountered at the ice-rock interface, clear evidence that the bottom of the ice sheet is...

Arthur A. Theisen; Glenn A. Borchardt; Moyle E. Harward; Roman A. Schmitt

1968-09-06T23:59:59.000Z

268

Teleconnections Between the Subtropical Monsoons and High-Latitude Climates During the Last Deglaciation  

Science Journals Connector (OSTI)

...peri-ods). The 1450-year and 1150-year periods have also been found in the 5180 (temper-ature) record of the Camp Century ice core in Greenland (33). Thus, all of the frequen-cies observed in the monsoonal climate ap-pear to be part...

F. Sirocko; D. Garbe-Schnberg; A. McIntyre; B. Molfino

1996-04-26T23:59:59.000Z

269

Effects of polar ice on the Earth's rotation and gravitational potential  

Science Journals Connector (OSTI)

......central ice cap were averaged to provide the time series for the latitudes 67"to 75", and the one ice core record at Camp Century in northwestern Greenland was used for the area north of 75"N Lat. As with the Antarctic ice cores, the means and......

Andrew S. Trupin

1993-05-01T23:59:59.000Z

270

The Origin of the Superstructure in Bi2Sr2CaCu2O8+? as Revealed by Scanning Tunneling Microscopy  

Science Journals Connector (OSTI)

...be identified and understood. Horibe et al. (1) originally reported that 02 trapped in 2000-year-old ice from Camp Century, Green-land, has an 180/160 enrichment given by 8 (180) = 0.61 per mil versus present-day at-mospheric...

M. D. Kirk; J. Nogami; A. A. Baski; D. B. Mitzi; A. Kapitulnik; T. H. Geballe; C. F. Quate

1988-12-23T23:59:59.000Z

271

Moonquakes  

Science Journals Connector (OSTI)

...basis of this work. The Greenland samples were from the Camp Century area (770l0'N, 61007'W) and from a virgin site...were recovered from the walls of an inclined shaft at Camp Century, and the sam-ples of more recent ages were taken...

G. Latham; M. Ewing; J. Dorman; D. Lammlein; F. Press; N. Toksoz; G. Sutton; F. Duennebier; Y. Nakamura

1971-11-12T23:59:59.000Z

272

Temperature profile for glacial ice at the South Pole: Implications for life in a nearby subglacial lake  

Science Journals Connector (OSTI)

...profiles of temperature vs. depth at Camp Century, Greenland, coincide to better...radian and 5.510 m/yr for Camp Century (7) and ?0.004 radian and 12.8...depth in the bottom part of the Camp Century and Byrd Station glaciers allows...

P. Buford Price; Oleg V. Nagornov; Ryan Bay; Dmitry Chirkin; Yudong He; Predrag Miocinovic; Austin Richards; Kurt Woschnagg; Bruce Koci; Victor Zagorodnov

2002-01-01T23:59:59.000Z

273

Antarctic Ice Sheet: Preliminary Results of First Core Hole to Bedrock  

Science Journals Connector (OSTI)

...unconsolidated sediment, such as glacial till, rather than solid rock. Glacial till underlies the Greenland ice sheet at Camp Century (4). Liquid water was encountered at the ice-rock interface, clear evidence that the bottom of the ice sheet is...

Anthony J. Gow; Herbert T. Ueda; Donald E. Garfield

1968-09-06T23:59:59.000Z

274

Superconducting and Magnetic Behavior in La2-xNaxCuO4  

Science Journals Connector (OSTI)

...this fabric (25). High strain rates and fluctu-ating stresses characterize the base ofthe Greenland ice sheet at Camp Century and Dye 3, but temperatures are less than-13 C and a single-maximum fabric is de-veloped (16-18, 24, 26...

M. A. SUBRAMANIAN; J. GOPALAKRISHNAN; C. C. TORARDI; T. R. ASKEW; R. B. FLIPPEN; A. W. SLEIGHT; J. J. LIN; S. J. POON

1988-04-22T23:59:59.000Z

275

Books Received  

Science Journals Connector (OSTI)

...of glacier ice is a relatively new aspect of glaciology that was stimulated by the retrieval of long ice cores from Camp Century in Green-land. Because seasonal variations in the physical characteristics of glacier ice diminish with depth, glaciologists...

1971-01-29T23:59:59.000Z

276

Science and its place in society  

Science Journals Connector (OSTI)

...Evidence in support of such a ma-jor ice mass has been provided by the analysis of the total gas content from the Camp Century ice core, which suggests that the northwest Greenland Ice Sheet was about 1300 m thicker than today to-ward the end...

EQ Daddario

1978-04-21T23:59:59.000Z

277

Surface-Related Mercury in Lunar Samples  

Science Journals Connector (OSTI)

...selenium content of these samples was determined by measurement of neutron induced 81Se. The samples were from the Camp Century area of the Greenland ice sheet (77 10'N and 61 07'W) and from a virgin area 80 km east southeast of this location...

G. W. Reed; J. A. Goleb; S. Jovanovic

1971-04-16T23:59:59.000Z

278

Nonequilibrium air clathrate hydrates in Antarctic ice: a paleopiezomdter for polar ice caps  

Science Journals Connector (OSTI)

...long as the ice thickness changes by only a few hundred meters. Examination of the deep ice cores from the Dye-3 and Camp Century sites in Greenland were made by the same microscopic thermal-needle method: at both these sites the onset of craigite...

H Craig; H Shoji; C C Langway; Jr

1993-01-01T23:59:59.000Z

279

Past Glacial Activity in the Canadian High Arctic  

Science Journals Connector (OSTI)

...CENTURIES OF CLIMATIC RECORD FROM CAMP CENTURY ON GREENLAND ICE SHEET, SCIENCE...OF TOTAL GAS CONTENT IN ICE AT CAMP CENTURY, NATURE 243 : 283 ( 1973 ). STEHLI...the total gas content from the Camp Century ice core, which suggests that...

J. England; R. S. Bradley

1978-04-21T23:59:59.000Z

280

Book Reviews  

Science Journals Connector (OSTI)

...of glacier ice is a relatively new aspect of glaciology that was stimulated by the retrieval of long ice cores from Camp Century in Green-land. Because seasonal variations in the physical characteristics of glacier ice diminish with depth, glaciologists...

1971-01-29T23:59:59.000Z

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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.


281

Simulating Arctic Climate Warmth and Icefield Retreat in the Last Interglaciation  

Science Journals Connector (OSTI)

...Meighen ice caps in the Canadian Arctic, and possibly in Camp Century (northwest Greenland), suggest that these drill sites were...marked S; 72.5N, 37.3W), and possibly Camp Century (marked C; 77.2N, 61.1W), but...

Bette L. Otto-Bliesner; Shawn J. Marshall; Jonathan T. Overpeck; Gifford H. Miller; Aixue Hu; CAPE Last Interglacial Project members

2006-03-24T23:59:59.000Z

282

When Will the Present Interglacial End?  

Science Journals Connector (OSTI)

...Some data indicate how rapid the cooling could have been near the end of an interglacial. In the Greenland ice core (Camp Century) a spectacular drop in 180 values appears to have oc-curred within a time interval only about 100 years long. The...

G. J. Kukla; R. K. Matthews

1972-10-13T23:59:59.000Z

283

Glacier in Chile Ended a Major Readvance about 36,000 Years Ago: Some Global Comparisons  

Science Journals Connector (OSTI)

...sharp cooling-41,000 calendar years ago on their revised (but still tentative) time scale for the ice core from Camp Century, Greenland, may correspond to the stade between the Port Talbot and Plum Point interstades, which Goldthwait et al...

J. H. Mercer; C. A. Laugenie

1973-12-07T23:59:59.000Z

284

A 2000-Year Tree Ring Record of Annual Temperatures in the Sierra Nevada Mountains  

Science Journals Connector (OSTI)

...temperature record (5) and may be related to a volcanic erup-tion that is recorded in the acidity record from the Camp Century, Greenland, ice core and in historical records (16). Effects of volcanic eruptions have been shown to influence...

Louis A. Scuderi

1993-03-05T23:59:59.000Z

285

Holocene dynamics of the Arctic's largest ice shelf  

Science Journals Connector (OSTI)

...24 . 27 Johnsen SF ( 2001 ) Oxygen isotope and paleotemperature records from six Greenland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland and NorthGRIP . J Quat Sci 16 : 299 307 . 28 Trees CC Clarke DK Bidigare RR Ondrusek ME Mueller...

Dermot Antoniades; Pierre Francus; Reinhard Pienitz; Guillaume St-Onge; Warwick F. Vincent

2011-01-01T23:59:59.000Z

286

Solar-Climate Relationships in the Post-Pleistocene  

Science Journals Connector (OSTI)

...years in the periodicity of glacial advance (2, 3) and in the temperature-related 8180 data from the Greenland Camp Century ice core (4). There is evidence that these cycles are based on 1242 face were removed for each incident solar wind...

J. Roger Bray

1971-03-26T23:59:59.000Z

287

Earth's early atmosphere  

Science Journals Connector (OSTI)

...cores from which greenhouse gases have been measured. Camp Century and Dye 3 are from Greenland, the other cores are from...temperature (g cm-2Year (in) ~~~~(00) yr1) Camp Century 1387 1966 1885-24 32 Dye 3 2037 1981 2480-19.6...

JF Kasting

1993-02-12T23:59:59.000Z

288

HoloceneLate Pleistocene Climatic Ice Core Records from Qinghai-Tibetan Plateau  

Science Journals Connector (OSTI)

...LGS-Holocene transition in the Camp Century core from northern Greenland...from polar cores. In cores from Camp Century (5) and Dye 3 (13) in Green-land...than the change of 11 per mil at Camp Century, 8 per mil at Devon Island, and...

L. G. THOMPSON; E. MOSLEY-THOMPSON; M. E. DAVIS; J. F. BOLZAN; J. DAI; L. KLEIN; T. YAO; X. WU; Z. XIE; N. GUNDESTRUP

1989-10-27T23:59:59.000Z

289

Globally synchronous ice core volcanic tracers and abrupt cooling during the last glacial period  

E-Print Network (OSTI)

Globally synchronous ice core volcanic tracers and abrupt cooling during the last glacial period R (2006), Globally synchronous ice core volcanic tracers and abrupt cooling during the last glacial period histories from ice coring of Greenland and Antarctica over the period 2 to 45 ka, using SO4 anomalies

Price, P. Buford

290

E-Print Network 3.0 - anel da valva Sample Search Results  

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

PhoTomonTage: daTagr af... . mobile AnD sUsTAinAble Dwellings in greenlAnD's vAcUUm solAr collecTor solAr pAnels solAr-heATeD ch... . The red triangle is the entrance, and the...

291

Influx Measurements of Extraterrestrial Material  

Science Journals Connector (OSTI)

...sedimentation rate, and influx. Fire-man and Langway (40...water-soluble Greenland fraction collected with ion-exchange...g of a nonmag-netic fraction of the clay, similar...rates for the unmelted fraction. Unfortunately we do...mate-rial with meteoritic release like that, for example...

David W. Parkin; David Tilles

1968-03-01T23:59:59.000Z

292

ANNUAL REVIEW 2012 director's summary  

E-Print Network (OSTI)

designed the drill based on the Danish drill used in Greenland for the NEEM ice coring project. The project authorities, government agencies, industry, and international Antarctic and climate change stakeholders. I am always impressed by the skill and enthusiasm, not to mention the time and energy, our researchers put

293

Annual Report 2010 Aarhus University  

E-Print Network (OSTI)

: The Danish Energy Agency The Environmental Protection Agency The Government of Greenland Private foundations4th Annual Report 2010 Aarhus University DCE ­ Danish Centre for Environment and Energy #12: Aarhus University, DCE ­ Danish Centre for Environment and Energy URL: http://dmu.au.dk Year

Schierup, Mikkel Heide

294

The Design of an Uninhabited Air Vehicle for Remote Sensing in the Cryosphere  

E-Print Network (OSTI)

, the design mission of this aircraft, named the Meridian, is to takeoff from a remote base camp in either Antarctica or Greenland, fly to some area of interest, acquire data such as ice thickness and surface elevation with ground penetrating radar, then return...

Donovan, William

2007-12-18T23:59:59.000Z

295

Marine and Petroleum Geology 24 (2007) 5366 An improved tectonic model for the Eocene opening of the  

E-Print Network (OSTI)

history of the North Atlantic, as the opening of the Norwegian­Greenland Sea between the Jan Mayen of Norway acquired a new aeromagnetic survey offshore Lofoten in 2003 and merged these data with reprocessed. Reprocessed gravity data were also used in the study. The new aeromagnetic grid and structural elements

Torsvik, Trond Helge

296

A Tracer Investigation oftheAtmosph^c Dispersion  

E-Print Network (OSTI)

Laboratory Erik Lyck Air Pollution Laboratory National Agency of Environmental Protection Abstract. Mining at Kvanefjeld, Greenland, will result in releases of air polluting gases. In order to measure the dilution and a sea-breeze. INIS-descriptors: AIR POLLUTION; DILUTION; DISPERSION; ENVIRONMENTAL IMPACTS; GASES

297

Understanding theUnderstanding the Polar RegionsPolar Regions in Climate Changein Climate Change  

E-Print Network (OSTI)

in the oceans and the atmosphere? #12;4 68 100 Gulf Stream Two ways to move heat : Ocean currents Atlantic Current provides about 60% of the inflow to the Arctic Ocean bringing warmer water from the Arctic Ocean through the passage between Greenland and Spitsbergen. http://www.aquatic.uoguelph.ca/oceans/ArticOceanWeb/Currents

Mountziaris, T. J.

298

H A&S 222d Spring 2009 Syllabus and logistics Tues-Thurs 10.30-12.20 MGH 284 labs: Oceanography  

E-Print Network (OSTI)

to mech. energy Diamond and Arctic peoples chemical bonding, chemical energy Siberian Arctic heat engine Sverdrup phase change: ice, water, steam Greenland's success and failure Alaska's natives and oil 4 20 solving energy in foods are we running out of food? traditional native diet, hunting and fishing the `eat'-engine

299

H A&S 222d/253e Spring 2007 Syllabus and logistics MWF 10.30-11.20 + labs/problem sessions MGH 242 OTB 206 (ocean)  

E-Print Network (OSTI)

Diamond and Arctic peoples chemical bonding, chemical energy Siberian Arctic heat engine Sverdrup phase change: ice, water, steam Greenland's success and failure Alaska's natives and oil 4 16/20 iv energy of food? traditional native diet, hunting and fishing the `eat'-engine Brown quiz 6 30iv/4 v

300

Intercontinental dispersal by a microendemic burrowing reptile (Dibamidae)  

Science Journals Connector (OSTI)

...of North Atlantic land bridges. In Structure and development...Greenland-Scotland bridge: new concepts and methods (eds M. H. P. Bott, S. Saxov...Plenum. 2 Tiffney, B. H. 1985 The Eocene North Atlantic land bridge: its importance in tertiary...

2011-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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.


301

F O R G I N G T H E L I N K 4-1 Historic and Projected  

E-Print Network (OSTI)

concentrations of CO2 gas trapped in Greenland and Antarctic ice. While historically, CO2 levels very seldom, including CO2 . A warming atmosphere allows it to hold greater amounts of water vapor, which in turn gasses like carbon dioxide (CO2 ) are well-documented and understood. · The atmospheric buildup of CO2

302

J. Phys. B AL Mol. Opt Phys. 26 (1993) 1569-1578. Printed in the UK Pure and mixed state calculationsof the laser-induced  

E-Print Network (OSTI)

, altemative methods for separating the elements of uranium are being studied, notably the use of lasers of the isotopes of uranium has major commercial importance in the nuclear fuel industry. As is well known to induce preferential ionization of 23sU(see Greenland 1991 for a review). Laser isotope separation relies

Ford, Ian

303

PART I THE POLICY CHALLENGES CLIMATE CHANGE  

E-Print Network (OSTI)

parts of the West Antarctic and Greenland ice sheets could catastrophically raise sea levels by over 1 already been released, and because the green- house gases (GHG) that cause climate change stay unless techno- logical advances enable us to extract GHGs from the atmosphere.The Intergovernmental Panel

304

The feeding ecology of little auks raises questions about winter zooplankton stocks in North Atlantic surface waters  

Science Journals Connector (OSTI)

...individual daily energy expenditure of 438...euphausiid/fish consumption, as well as the...regional food webs and energy flow. Figure-1...Figure-2. Average number of dives...of the Greenland Home Rule Government...numbers and prey consumption in the North Atlantic...

2010-01-01T23:59:59.000Z

305

Behaviour and kinematics of continuous ram filtration in bowhead whales (Balaena mysticetus)  

Science Journals Connector (OSTI)

...speed to maximize net energy gain. This implies...food uptake with energy consumption and oxygen assimilation...concentrations to save energy when food concentrations...densities than found on average, suggests that bowhead...KIIIN, Greenlandic Home Rule, P.T.M...

2009-01-01T23:59:59.000Z

306

Riso Report No. 132 Danish Atomic Energy Commission  

E-Print Network (OSTI)

Riso Report No. 132 B ! Danish Atomic Energy Commission Research Establishment Riso Environmental. Stilvfade, Copenhagen K.r Denmark A vailffbt? on exchangtfrom: Library, t>»«ijh Atomic Energy Commission Radioactivity in Greenland in 1965 by A. Aarkrog and J. Lippert The Danish Atomic Energy Commission Research

307

U.S. District Court: Vermont Auto Dealers & Manufacturers versus  

E-Print Network (OSTI)

on Greenland #12;Areas Under Water: Four Regions #12;Paleoclimate Sea Level Data 1. Rate of Sea Level Rise - Data reveal numerous cases of rise of several m/century (e.g., MWP 1A) 2. "Sub-orbital" Sea Level greenhouse gas emissions... "...at a level that would prevent dangerous anthropogenic interference

Hansen, James E.

308

Amer J of Potato Res (2006) 83:249-257 249 Furrow vs Hill Planting of Sprinkler-Irrigated Russet Burbank  

E-Print Network (OSTI)

Amer J of Potato Res (2006) 83:249-257 249 Furrow vs Hill Planting of Sprinkler-Irrigated Russet Burbank Potatoes on Coarse-Textured Soils Dean D. Steele1 *, Richard G. Greenland2 , and Harlene M Surface water runoff from the hill, where potatoes are planted, to the furrow may exacerbate potato

Steele, Dean D.

309

A Fish from the Upper Cambrian of North America  

Science Journals Connector (OSTI)

...occur-rences ofAnatolepis in North America, Greenland...years ago) (1, 2). In 1976 and 1977...in Crook County, north-eastern Wyoming...specific gravity _ 2.9; specific gravity...Cambrian-Ordovician North American paleocontinent...vertebrates (1, 2, 19). JOHN E...

JOHN E. REPETSKI

1978-05-05T23:59:59.000Z

310

Dynamics of the sea ice edge in Davis Strait M.P. Heide-Jrgensen a,, H. Stern b  

E-Print Network (OSTI)

on the banks of West Greenland, sea ice produced further north in Baffin Bay was advected to the banks as shownAuthor's personal copy Dynamics of the sea ice edge in Davis Strait M.P. Heide-Jørgensen a,, H October 2006; accepted 27 October 2006 Available online 22 December 2006 Abstract Sea ice concentration

Laidre, Kristin L.

311

New ice core evidence for a volcanic cause of the A.D. 536 dust veil  

E-Print Network (OSTI)

New ice core evidence for a volcanic cause of the A.D. 536 dust veil L. B. Larsen,1 B. M. Vinther,1. [1] New and well-dated evidence of sulphate deposits in Greenland and Antarctic ice cores indicate a substantial and extensive atmospheric acidic dust veil at A.D. 533­534 ± 2 years. This was likely produced

Nicolussi, Kurt

312

/ http://www.sciencemag.org/content/early/recent / 17 April 2014 / Page 1/ 10.1126/science.1249047 A diverse set of geochemical records has been developed from ice re-  

E-Print Network (OSTI)

silty ice. This isotope is contin- uously produced by cosmic rays in the atmosphere, is delivered.1249047 A diverse set of geochemical records has been developed from ice re- covered in the 3054-m Greenland Ice Sheet Project 2 (GISP2) core. These data provide a detailed history of climate and ice

Napp, Nils

313

IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, VOL. 37, NO. 3, MAY 1999 1671 Cryosphere Applications of NSCAT Data  

E-Print Network (OSTI)

IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, VOL. 37, NO. 3, MAY 1999 1671 Cryosphere covering Greenland and Antarctica add to the polar heat sink effect by their additional influence upon. Hence, monitoring of polar ice is of particular interest to the remote sensing and climate change

Long, David G.

314

VLF/LF reflectivity of the polar ionosphere. Report for 2 September-22 December 1979  

SciTech Connect

This report provides a summary of high latitude ionospheric reflectivity as observed by the USAF high resolution VLF/LF ionosounder operating in northern Greenland. Ionospheric reflectivity parameters, including reflection heights and coefficients, are presented as a function of time of day. Riometer and magnetometer measurements of the polar propagation environment are presented as supplementary data.

Pagliarulo, R.P.; Turtle, J.P.; Rasmussen, J.E.; Klemetti, W.I.

1980-06-01T23:59:59.000Z

315

Gas ageice age differences and the chronology of the Vostok ice core, M. L. Bender,1  

E-Print Network (OSTI)

Gas age­ice age differences and the chronology of the Vostok ice core, 0­100 ka M. L. Bender,1 G. [1] Gas is trapped in polar ice at depths of $50­120 m and is therefore significantly younger than cores (Vostok, Dome Fuji, and Dome C). We recorrelate the gas records of Vostok and Greenland Ice Sheet

Chappellaz, Jérôme

316

Contrasting the regional Arctic System Reanalysis with the global ERA-Interim Reanalysis+  

E-Print Network (OSTI)

development and localized wind phenomena, a cyclone case study and data from the Greenland Flow Distortion for near-surface temperature, dewpoint, pressure, and wind speed, but RMSE and correlations significantly, and wind speed are very small compared to radiosonde data. ASR demonstrates lower RMSEs and higher

Howat, Ian M.

317

First report of Wiwaxia from the Cambrian Chengjiang Lagersttte  

E-Print Network (OSTI)

Greenland and their role in early protostome evolution. Philosophical Transactions of the Royal Society of London, Series B 347, 30558. CONWAY MORRIS, S. & ROBISON, R. A. 1988. More soft-bodied animals and algae from the Middle Cambrian of Utah...

Zhao, Fang-Chen; Smith, Martin R.; Yin, Zong-Jun; Zeng, Han; Hu, Shi-Xue; Li, Guo-Xiang; Zhu, Mao-Yan

2014-01-01T23:59:59.000Z

318

Serpentinite and the dawn of life  

Science Journals Connector (OSTI)

...approximately 3.8 Ga [72], Nuvvuagittuq (Canada) at 3.75 Ga [96] and Akilia (Greenland...approximately 4.0 Ga Acasta Gneiss Complex in Canada and subsequent authors have repeated this...specifically, the advent of harvesting solar energy into Earth's geochemical cycles...

2011-01-01T23:59:59.000Z

319

Ris Ris-M-GSZJ Title and authors)  

E-Print Network (OSTI)

Risø Risø-M-GSZJ Title and authors) External Radiation Exposure Associated with Uranium Nielsen * . +) The Geological Survey of Greenland 11 pages + 3 tables + 2 illustrations Date February 19 radia- tion levels because of extensive uranium and thorium mineralizations. The measuring programme

320

-> Rise Report No. 355 Ris National Laboratory  

E-Print Network (OSTI)

Survey 5 2. I. Geology and Mineralogy of the Ore 5 2. 2. Recovery of Uranium, Choice of Method 11 2 of a Greenlandic Uranium Ore, F Reactivity of Minerals and Recovery o o \\J by J. K. Gamborg Hansen ft March 1977 REFRACTORIES ROASTING SULFATES SULFUR OXIDES THERMAL GRAVIMETRIC ANALYSIS URANIUM ORES X-RAY DIFFRACTION UDC

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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.


321

Ris Report No. 375 5 Ris National Laboratory  

E-Print Network (OSTI)

NEUTRON ANALYSIS URANIUM URANIUM MINERALS [JJ ABSORPTION SPECTROSCOPY COPPER LEAD VANADIUM ZINC UDC 550, Rheinisch-Westfalische Technische Hochschule, D-51 Aachen, West Germany. The Geological Survey of Greenland;#12;5 CONTENTS Page 1. INTRODUCTION 7 2. GEOLOGY AND MINERALISATION 9 3. SAMPLING AND ANALYSIS 11 3.1. Sampling

322

A Geostatistical Study of the Uranium Deposit at Kvanefjeld,  

E-Print Network (OSTI)

with the geology. It is also shown that, although anisotropy exists, the uranium variation has a secondRisa-R-468 A Geostatistical Study of the Uranium Deposit at Kvanefjeld, The Ilimaussaq Intrusion A GEOSTATISTICAL STUDY OF THE URANIUM DEPOSIT AT KVANEFJELD, THE ILIMAUSSAQ INTRUSION, SOUTH GREENLAND Flemming

323

Ann. Geophys., 28, 155163, 2010 www.ann-geophys.net/28/155/2010/  

E-Print Network (OSTI)

flow in North America, windstorms in Norway in westerly flow, Greenland wind- storms in both westerly energy, TKE, and its dissipation rate, . The computation of is performed using the inertial dissipation con- siderations about defining turbulent perturbations of the bora wind velocity are also pointed out

Belusic, Danijel

324

Cassandra Wheeler Univ. of Colorado Department of Atmospheric and Oceanic Sciences (ATOC)  

E-Print Network (OSTI)

on the energy budget NOAA's Contribution: Remotely observe cloud layers and environmental conditions Svalbard, Norway 85 °N 0 °E Greenland Location: 87°N Duration: 1 Aug ­15 Sept 2008 Platform : Swedish Icebreaker Oden #12;Ka-Band Radar S-Band Radar Wind Profiler Scanning Radiometer Lidar Ceilometer 2-Channel

325

Bangladesh-Pilot Program for Climate Resilience (PPCR) | Open Energy  

Open Energy Info (EERE)

Bangladesh-Pilot Program for Climate Resilience (PPCR) Bangladesh-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Bangladesh-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Bangladesh UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

326

Zambia-Pilot Program for Climate Resilience (PPCR) | Open Energy  

Open Energy Info (EERE)

Zambia-Pilot Program for Climate Resilience (PPCR) Zambia-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Zambia-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Zambia UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

327

Jamaica-Pilot Program for Climate Resilience (PPCR) | Open Energy  

Open Energy Info (EERE)

Jamaica-Pilot Program for Climate Resilience (PPCR) Jamaica-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Jamaica-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Jamaica UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

328

Haiti-Pilot Program for Climate Resilience (PPCR) | Open Energy Information  

Open Energy Info (EERE)

Haiti-Pilot Program for Climate Resilience (PPCR) Haiti-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Haiti-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Haiti UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

329

Saint Lucia-Pilot Program for Climate Resilience (PPCR) | Open Energy  

Open Energy Info (EERE)

Saint Lucia-Pilot Program for Climate Resilience (PPCR) Saint Lucia-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Saint Lucia-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Saint Lucia UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

330

Mozambique-Pilot Program for Climate Resilience (PPCR) | Open Energy  

Open Energy Info (EERE)

Mozambique-Pilot Program for Climate Resilience (PPCR) Mozambique-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Mozambique-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Mozambique UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

331

Dominica-Pilot Program for Climate Resilience (PPCR) | Open Energy  

Open Energy Info (EERE)

Dominica-Pilot Program for Climate Resilience (PPCR) Dominica-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Dominica-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Dominica UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

332

Yemen-Pilot Program for Climate Resilience (PPCR) | Open Energy Information  

Open Energy Info (EERE)

Yemen-Pilot Program for Climate Resilience (PPCR) Yemen-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Yemen-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Yemen UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

333

Samoa-Pilot Program for Climate Resilience (PPCR) | Open Energy Information  

Open Energy Info (EERE)

Samoa-Pilot Program for Climate Resilience (PPCR) Samoa-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Samoa-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Samoa UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

334

Nepal-Pilot Program for Climate Resilience (PPCR) | Open Energy Information  

Open Energy Info (EERE)

Nepal-Pilot Program for Climate Resilience (PPCR) Nepal-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Nepal-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Nepal UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

335

Tajikistan-Pilot Program for Climate Resilience (PPCR) | Open Energy  

Open Energy Info (EERE)

Tajikistan-Pilot Program for Climate Resilience (PPCR) Tajikistan-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Tajikistan-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Tajikistan UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

336

Bolivia-Pilot Program for Climate Resilience (PPCR) | Open Energy  

Open Energy Info (EERE)

Bolivia-Pilot Program for Climate Resilience (PPCR) Bolivia-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Bolivia-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Bolivia UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

337

Niger-Pilot Program for Climate Resilience (PPCR) | Open Energy Information  

Open Energy Info (EERE)

Niger-Pilot Program for Climate Resilience (PPCR) Niger-Pilot Program for Climate Resilience (PPCR) Jump to: navigation, search Name Niger-Pilot Program for Climate Resilience (PPCR) Agency/Company /Organization World Bank Sector Energy, Land Topics Background analysis, Finance, Implementation, Low emission development planning, Market analysis Website http://www.climateinvestmentfu Country Niger UN Region Southern Asia References Pilot Program for Climate Resilience (PPCR)[1] Contents 1 Overview 2 Programs by Country 2.1 Bangladesh 2.2 Bolivia 2.3 Cambodia 2.4 Dominica 2.5 Grenada 2.6 Haiti 2.7 Jamaica 2.8 Mozambique 2.9 Nepal 2.10 Niger 2.11 Papua New Guinea 2.12 Saint Lucia 2.13 Saint Vincent and the Grenadines 2.14 Samoa 2.15 Tajikistan 2.16 Tonga 2.17 Yemen 2.18 Zambia 3 References Overview "The Pilot Program for Climate Resilience (PPCR), approved in November

338

Effect of ocean temperature on southwestern U.S. climate analyzed  

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

Effect of ocean temperature on southwestern climate Effect of ocean temperature on southwestern climate Effect of ocean temperature on southwestern U.S. climate analyzed Researchers concluded that only part of the recent temperature rise in the Southwest could be attributed to greenhouse gases. December 19, 2013 Image from National Oceanic and Atmospheric Administration's Environmental Visualization Laboratory depicts sea surface temperatures around Greenland from October 2010. Image from National Oceanic and Atmospheric Administration's Environmental Visualization Laboratory depicts sea surface temperatures around Greenland from October 2010. Assuming that the past is a good indicator of the future, the scientists conclude that there should be wetter times ahead. Researchers have analyzed the relationship between a natural phenomenon in

339

Moulin bleu  

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

Moulin bleu Moulin bleu 1663 Los Alamos science and technology magazine Latest Issue:November 2013 All Issues » submit Moulin bleu Tunneling meltwater rivers enlarged by climate change help shuttle glacial ice to the sea less than previously thought. November 25, 2013 Moulin bleu Meltwater on the Greenland ice sheet forms surface flows that can eventually dive into moulins. These moulins deliver water to the base of the ice sheet, where it marginally affects the rate at which glaciers move to the sea. (CREDIT: Matthew Hoffman/LANL) A rare morsel of good news about sea-level rise from the Greenland ice sheet As major ice sheets melt and flow into the ocean-a process accelerated by climate change-the global sea level rises. This process is further sped up by the meltwater lubrication effect, in which meltwater rivers tunnel

340

Glacier Girl flies again | Y-12 National Security Complex  

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Glacier Girl flies again Glacier Girl flies again Glacier Girl flies again Posted: February 11, 2013 - 3:42pm | Y-12 Report | Volume 9, Issue 2 | 2013 On July 15, 1942, foul weather forced six P-38 fighters and two B-17 bombers to crash-land on Greenland. The squadron's crew, en route from Maine to England to support Allied war efforts, was rescued, but the aircraft were left behind on the arctic ice cap. For 50 years, an ice and snow cocoon enveloped six P-38 fighters and two B-17 bombers that crash-landed on Greenland during World War II. Then, in 1992, after 12 failed attempts to recover the planes, a group of adventurers tunneled through 268 feet of packed ice and raised one of the P-38 fighters piece by piece. Once brought to the surface, the sections were flown to Middlesboro, Ky. - home of the project's financier, Roy

Note: This page contains sample records for the topic "greenland grenada guadeloupe" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
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We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


341

Aerosol and graphitic carbon content of snow  

SciTech Connect

Snow samples from southern New Mexico, west Texas, Antarctica, and Greenland were analyzed for aerosol and graphitic carbon. Graphitic carbon contents were found to be between 2.2 and 25 ..mu..g L/sup -1/ of snow meltwater; water-insoluble aerosol content varied between 0.62 and 8.5 mg L/sup -1/. For comparison, two samples of Camp Century, Greenland, ice core, having approximate ages of 4,000 and 6,000 years, were also analyzed. Ice core graphitic carbon contents were found to be 2.5 and 1.1 ..mu..g L/sup -1/. copyrightAmerican Geophysical Union 1987

Chy-acute-accentlek, P.; Srivastava, V.; Cahenzli, L.; Pinnick, R.G.; Dod, R.L.; Novakov, T.; Cook, T.L.; Hinds, B.D.

1987-08-20T23:59:59.000Z

342

Circumpolar Study of Perfluoroalkyl Contaminants in Polar Bears (Ursus maritimus)  

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Box 570, DK-3900 Nuuk, Greenland, Denmark, University of Alberta, Edmonton, Alberta, Canada, National Wildlife Research Centre, Environment Canada, Ottawa, Ontario, Canada, United States Fish and Wildlife Service, 1011 East Tudor Road, Anchorage, Alaska 99503, Department of Sustainable Development, Government of Nunavut, Iqaluit, Nunavut, Canada, Canadian Wildlife Service, Environment Canada, Edmonton, Alberta T6B 2X3, Canada, Department of Resources, Wildlife and Economic Development, Government of the Northwest Territories, Inuvik, Northwest Territories, Canada, and National Water Research Institute, Environment Canada, 867 Lakeshore Road, Burlington, Ontario L7R 4A6, Canada ... If PFAs (and/or precursors) are being transported via wind and/or ocean currents, then the prevailing pathways suggest that the source of the PFAs in the European Arctic and eastern Greenland would be attributable to transport from Western Europe and eastern North America, while the Western North American Arctic would be influenced mainly by East Asian sources (24). ...

Marla Smithwick; Scott A. Mabury; Keith R. Solomon; Christian Sonne; Jonathan W. Martin; Erik W. Born; Rune Dietz; Andrew E. Derocher; Robert J. Letcher; Thomas J. Evans; Geir W. Gabrielsen; John Nagy; Ian Stirling; Mitch K. Taylor; Derek C. G. Muir

2005-06-22T23:59:59.000Z

343

Bore-hole survey at Camp Century, 1989  

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A combination of the directional surveys of the Camp Century borehole from 1966, 1967, 1969 and 1989 has revealed a deformation pattern similar to that measured at Dye-3, South Greenland and Byrd Station, Antarctica showing high deformation rate for Wisconsin ice. Compared to the Dye-3 profile, the deformation shows the same pattern even in details. The surface velocity obtained by integrating the bore hole deformation is in agreement with that obtained from satellite measurements.

N.S Gundestrup; D Dahl-Jensen; B.L Hansen; J Kelty

1993-01-01T23:59:59.000Z

344

Particulate Matter in Antarctic Snow  

Science Journals Connector (OSTI)

......1 8.0 0.35 7.2 0.080 Camp Century (Greenland 77" N 61"W) 37...1 Amundsen-Scott 1 Plateau 1 Camp Century 1 SeaWater(Na 1.05%) 1 Terrestrial...1-3 4.0 6.9 0.35 7.2 Camp Century 0 4.7 37 21 0.027 10.6 0......

D. W. Parkin; D. R. Phillips

1972-05-01T23:59:59.000Z

345

Doubling of atmospheric methane supported  

SciTech Connect

Atmospheric methane over the past 27,000 years was measured by analyzing air trapped in glacial ice in Greenland and Antarctica. Atmospheric concentrations were stable over that period until about 200 years b.p. In the last 200 years they have more than doubled. This change in concentration is correlated with the increase in human population; the implications for climate modification are discussed. 1 figure, 3 references.

Kerr, R.A.

1984-11-23T23:59:59.000Z

346

Bioaccessibility and Transport by Caco-2 Cells of Organoarsenical Species Present in Seafood  

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Bioaccessibility and Transport by Caco-2 Cells of Organoarsenical Species Present in Seafood ... Organoarsenical standards and raw and cooked seafood (DORM-2, sole, and Greenland halibut) were subjected to in vitro gastrointestinal digestion to estimate arsenic bioaccessibility (maximum soluble concentration in gastrointestinal medium). ... In seafood, bioaccessibility was 67.5?100% for arsenobetaine (AB), 30% for dimethylarsinic acid (DMA), 45% for tetramethylarsonium ion (TETRA), and >50% for trimethylarsine oxide (TMAO). ...

J. M. Laparra; D. Vlez; R. Barber; R. Montoro; R. Farr

2007-06-13T23:59:59.000Z

347

An update on land-ice modeling in the CESM  

SciTech Connect

Mass loss from land ice, including the Greenland and Antarctic ice sheets as well as smaller glacier and ice caps, is making a large and growing contribution to global sea-level rise. Land ice is only beginning to be incorporated in climate models. The goal of the Land Ice Working Group (LIWG) is to develop improved land-ice models and incorporate them in CESM, in order to provide useful, physically-based sea-level predictions. LJWG efforts to date have led to the inclusion of a dynamic ice-sheet model (the Glimmer Community Ice Sheet Model, or Glimmer-CISM) in the Community Earth System Model (CESM), which was released in June 2010. CESM also includes a new surface-mass-balance scheme for ice sheets in the Community Land Model. Initial modeling efforts are focused on the Greenland ice sheet. Preliminary results are promising. In particular, the simulated surface mass balance for Greenland is in good agreement with observations and regional model results. The current model, however, has significant limitations: The land-ice coupling is one-way; we are using a serial version of Glimmer-CISM with the shallow-ice approximation; and there is no ice-ocean coupling. During the next year we plan to implement two-way coupling (including ice-ocean coupling with a dynamic Antarctic ice sheet) with a parallel , higher-order version of Glimmer-CISM. We will also add parameterizations of small glaciers and ice caps. With these model improvements, CESM will be able to simulate all the major contributors to 21st century global sea-level rise. Results of the first round of simulations should be available in time to be included in the Fifth Assessment Report (ARS) of the Intergovernmental Panel on Climate Change.

Lipscomb, William H [Los Alamos National Laboratory

2011-01-18T23:59:59.000Z

348

The camp century 10Be record: Implications for long-term variations of the geomagnetic dipole moment  

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10Be concentrations measured in ice samples from Camp Century, Greenland, show short term variations which in general correspond to the 100200 year wiggles in the 14C tree ring record. There is, however, no evidence for a long term variation over the last 5000 years. This constancy is in contrast to the approximately sinusoidal variation of the atmospheric 14C concentration which has generally been attributed to a changing geomagnetic dipole moment. This discrepancy implies that the 14C trend might stem from other causes such as changes of oceanic circulation processes or from higher production rates during the Wisconsin rather than from variation in the geomagnetic field.

Jrg Beer; Michael Andree; Hans Oeschger; Ulrich Siegenthaler; G. Bonani; H. Hofmann; E. Morenzoni; M. Nessi; M. Suter; W. Wlfli; R. Finkel; C. Langway Jr.

1984-01-01T23:59:59.000Z

349

LANL Mobile News  

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Reliability Technology earns prestigious Los Alamos award Reliability Technology earns prestigious Los Alamos award LANL has honored Michael Hamada, Harry Martz and a team of researchers with its first Richard Feynman Prize for Innovation Achievement.08/27/13 New gamma-ray observatory begins operations at Sierra Negra volcano in the state of Puebla, Mexico The High-Altitude Water Cherenkov Gamma Ray Observatory has begun formal operations at its site in Mexico.08/21/13 Meltwater effects on flow of Greenland's ice sheet less severe for sea level rise than earlier feared, scientists say The team found that accelerating ice sheet movement from increasing meltwater lubrication is likely to have only a minor role in future sea-level rise.08/19/13 Little Boy weaponeer William "Deak" Parsons, wartime Los Alamos

350

Geoengineering: Plan B Remedy for Global Warming Andrew A. Lacis  

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Geoengineering: Plan B Remedy for Global Warming Geoengineering: Plan B Remedy for Global Warming Andrew A. Lacis NASA Goddard Institute for Space Studies Accelerated melting of Greenland ice is a clear indication that consequences of global warming are real and impending. The underlying causes of global warming are well enough understood, but the necessary reduction of greenhouse gases to prevent irreversible climate change is unlikely to happen before the point of no return is reached. To reverse the impending sea level rise, geoengineering counter- measures may be required to counter the current global energy imbalance due to global warming. Of the many proposed remedies, deploying aerosols within the stratosphere offers realistic prospects. Sulfur injections in the lower stratosphere would have the cooling effect of naturally occurring volcanic aerosols. Soot at

351

NPP Tropical Forest: Kade, Ghana  

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Kade, Ghana, 1957-1972 Kade, Ghana, 1957-1972 [PHOTOGRAPH] Photograph: Forest after clearing of secondary growth at the Kade site (click on the photo to view a series of images from this site). Data Citation Cite this data set as follows: Nye, P. H., and D. J. Greenland. 1998. NPP Tropical Forest: Kade, Ghana, 1957-1972. Data set. Available on-line [http://www.daac.ornl.gov] from Oak Ridge National Laboratory Distributed Active Archive Center, Oak Ridge, Tennessee, U.S.A. Description Biomass and nutrient content of different vegetation components and soil for a secondary tropical forest were determined in the late 1950s at the Kade Agricultural Research Station of the former University College, Ghana. Net primary production (NPP) was estimated on the basis of standing biomass accumulation and litter fall. Later studies on litter and wood fall and

352

幻灯片 1  

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TSINGHUA TSINGHUA UNIVERSITY CCS related research activities in 3E (Energy, Environment and Economy Research Institute), Tsinghua Univ. Dr. Ruina XU, Prof. Wenying CHEN & Prof. Zongxin WU Tsinghua University May 30, 2008 TSINGHUA UNIVERSITY Outline * CCS related research projects - EU FP6 project -- Geocapacity - EU FP6 project -- COACH - Sino-UK cooperation -- NZEC - Sino-US cooperation * Progress of these projects TSINGHUA UNIVERSITY EU FP6 project -- GeoCapacity TSINGHUA UNIVERSITY GeoCapacity Partic. Number Participant Name Participant Short name Country 1 Geological Survey of Denmark and Greenland GEUS Denmark 2 University of Sofia US Bulgaria 3 University of Zagreb RGN Croatia 4 Czech Geological Survey CGS Czech Republic 5 Institute of Geology at Tallinn University of Technology IGTUT Estonia

353

Time varying arctic climate change amplification  

SciTech Connect

During the past 130 years the global mean surface air temperature has risen by about 0.75 K. Due to feedbacks -- including the snow/ice albedo feedback -- the warming in the Arctic is expected to proceed at a faster rate than the global average. Climate model simulations suggest that this Arctic amplification produces warming that is two to three times larger than the global mean. Understanding the Arctic amplification is essential for projections of future Arctic climate including sea ice extent and melting of the Greenland ice sheet. We use the temperature records from the Arctic stations to show that (a) the Arctic amplification is larger at latitudes above 700 N compared to those within 64-70oN belt, and that, surprisingly; (b) the ratio of the Arctic to global rate of temperature change is not constant but varies on the decadal timescale. This time dependence will affect future projections of climate changes in the Arctic.

Chylek, Petr [Los Alamos National Laboratory; Dubey, Manvendra K [Los Alamos National Laboratory; Lesins, Glen [DALLHOUSIE U; Wang, Muyin [NOAA/JISAO

2009-01-01T23:59:59.000Z

354

Echo?Ranging Device Used to Measure the Size of a Well at Camp Century  

Science Journals Connector (OSTI)

The echo?ranging device used to determine the size of a heat?sink well at Camp Century Greenland is briefly described. A rotating bariumtitanate narrow?beam transducer served as both transmitter and receiver. Short 500?kc/sec acoustic pulses were generated at the transducer by shock excitation. The device was designed to operate to a maximum range of 500 ft when suspended from a 1200?ft cable. A graphic recorder presented the echo time as a horizontal cross section of the well. The configuration of the well was determined by repeating the horizontal scan at successive depths. Tests at Camp Century revealed that the well was approximately 200 ft in diam with a water depth of approximately 100 ft. Good repeatability and an accuracy of less than 6 in. was demonstrated. The volume of the well was determined to be approximately 2 million cu ft. [Work supported by the U. S. Army.

O. Charles Mullineaux

1964-01-01T23:59:59.000Z

355

Low time resolution analysis of polar ice cores cannot detect impulsive nitrate events  

E-Print Network (OSTI)

Ice cores are archives of climate change and possibly large solar proton events (SPEs). Wolff et al. (2012) used a single event, a nitrate peak in the GISP2-H core, which McCracken et al. (2001a) time associated with the poorly quantified 1859 Carrington event, to discredit SPE-produced, impulsive nitrate deposition in polar ice. This is not the ideal test case. We critique the Wolff et al. analysis and demonstrate that the data they used cannot detect impulsive nitrate events because of resolution limitations. We suggest re-examination of the top of the Greenland ice sheet at key intervals over the last two millennia with attention to fine resolution and replicate sampling of multiple species. This will allow further insight into polar depositional processes on a sub-seasonal scale, including atmospheric sources, transport mechanisms to the ice sheet, post-depositional interactions, and a potential SPE association.

Smart, D F; Melott, A L; Laird, C M

2015-01-01T23:59:59.000Z

356

A multi-model assessment of pollution transport to the Arctic  

SciTech Connect

We examine the response of Arctic gas and aerosol concentrations to perturbations in pollutant emissions from Europe, East and South Asia, and North America using results from a coordinated model intercomparison. These sensitivities to regional emissions (mixing ratio change per unit emission) vary widely across models and species. Intermodel differences are systematic, however, so that the relative importance of different regions is robust. North America contributes the most to Arctic ozone pollution. For aerosols and CO, European emissions dominate at the Arctic surface but East Asian emissions become progressively more important with altitude, and are dominant in the upper troposphere. Sensitivities show strong seasonality: surface sensitivities typically maximize during boreal winter for European and during spring for East Asian and North American emissions. Mid-tropospheric sensitivities, however, nearly always maximize during spring or summer for all regions. Deposition of black carbon (BC) onto Greenland is most sensitive to North American emissions. North America and Europe each contribute {approx}40% of total BC deposition to Greenland, with {approx}20% from East Asia. Elsewhere in the Arctic, both sensitivity and total BC deposition are dominated by European emissions. Model diversity for aerosols is especially large, resulting primarily from differences in aerosol physical and chemical processing (including removal). Comparison of modeled aerosol concentrations with observations indicates problems in the models, and perhaps, interpretation of the measurements. For gas phase pollutants such as CO and O{sub 3}, which are relatively well-simulated, the processes contributing most to uncertainties depend on the source region and altitude examined. Uncertainties in the Arctic surface CO response to emissions perturbations are dominated by emissions for East Asian sources, while uncertainties in transport, emissions, and oxidation are comparable for European and North American sources. At higher levels, model-to-model variations in transport and oxidation are most important. Differences in photochemistry appear to play the largest role in the intermodel variations in Arctic ozone sensitivity, though transport also contributes substantially in the mid-troposphere.

Shindell, D T; Chin, M; Dentener, F; Doherty, R M; Faluvegi, G; Fiore, A M; Hess, P; Koch, D M; MacKenzie, I A; Sanderson, M G; Schultz, M G; Schulz, M; Stevenson, D S; Teich, H; Textor, C; Wild, O; Bergmann, D J; Bey, I; Bian, H; Cuvelier, C; Duncan, B N; Folberth, G; Horowitz, L W; Jonson, J; Kaminski, J W; Marmer, E; Park, R; Pringle, K J; Schroeder, S; Szopa, S; Takemura, T; Zeng, G; Keating, T J; Zuber, A

2008-03-13T23:59:59.000Z

357

The microstructure of polar ice. Part I: Highlights from ice core research  

Science Journals Connector (OSTI)

Abstract Polar ice sheets play a fundamental role in Earth's climate system, by interacting actively and passively with the environment. Active interactions include the creeping flow of ice and its effects on polar geomorphology, global sea level, ocean and atmospheric circulation, and so on. Passive interactions are mainly established by the formation of climate records within the ice, in form of air bubbles, dust particles, salt microinclusions and other derivatives of airborne impurities buried by recurrent snowfalls. For a half-century scientists have been drilling deep ice cores in Antarctica and Greenland for studying such records, which can go back to around a million years. Experience shows, however, that the ice-sheet flow generally disrupts the stratigraphy of the bottom part of deep ice cores, destroying the integrity of the oldest records. For all these reasons glaciologists have been studying the microstructure of polar ice cores for decades, in order to understand the genesis and fate of ice-core climate records, as well as to learn more about the physical properties of polar ice, aiming at better climate-record interpretations and ever more precise models of ice-sheet dynamics. In this Part I we review the main difficulties and advances in deep ice core drilling in Antarctica and Greenland, together with the major contributions of deep ice coring to the research on natural ice microstructures. In particular, we discuss in detail the microstructural findings from Camp Century, Byrd, Dye 3, GRIP, GISP2, NorthGRIP, Vostok, Dome C, EDML, and Dome Fuji, besides commenting also on the earlier results of some pioneering ventures, like the Jungfraujoch Expedition and the NorwegianBritishSwedish Antarctic Expedition, among others. In the companion Part II of this work (Faria etal., 2014), the review proceeds with a survey of the state-of-the-art understanding of natural ice microstructures and some exciting prospects in this field of research.

Srgio H. Faria; Ilka Weikusat; Nobuhiko Azuma

2014-01-01T23:59:59.000Z

358

NEWTON, Ask a Scientist at Argonne National Labs  

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Permanence of Ocean Currents Permanence of Ocean Currents Name: Teresia Status: student Grade: 6-8 Country: Tanzania Date: Winter 2011-2012 Question: Are ocean currents permanent? Replies: Teresia: Although many ocean currents have been around for many thousands or years, they can and do change over time. One of the problems some scientists see with global warming is that some currents may shift or stop all together. For example, some folks, are worried that much fresh water may flow into the sea from melting ice in Greenland This would, they say, stop the Gulf Stream in the Atlantic ocean which keeps Europe warm That would plunge Europe into another ice age. But, on the whole, ocean currents do not change over the life of a human being. Mr.Avakian Teresia, Since ocean currents are controlled by several factors: wind - which is the main cause of the different rotations in the northern and southern hemisphere, salinity - which, for example is the main factor in the southward diffusion from the north pole in the Atlantic ocean and the gulf stream, temperature, general ocean floor topography, etc. - changes (on a geological time scale) will cause changes in the ocean currents.

359

Lichens  

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Lichens Lichens Nature Bulletin No. 131 November 15, 1947 Forest Preserve District of Cook County William N. Erickson, President Roberts Mann, Supt. of Conservation LICHENS When winter comes with its fogs, rains, and melting snow, the lichens flourish. In the country we find them on the bark of trees, boulders and patches of barren earth, but rarely in cities because they are very sensitive to poisonous gases in the smoky air. In Iceland and Greenland, and the vast tundras of the arctics, they are the dominant forms of plant life. A lichen is the partnership of a colorless plant and a green one: a fungus and an alga. The two exchange food materials. Fungus has remarkable power to absorb and store moisture. The alga, using that water, and using carbon dioxide from the air, manufactures food. The fungus absorbs the excess food and produces an acid which eats into the earth or wood or rock upon which it grows, anchoring it firmly in place.

360

The Musk Ox  

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Musk Ox Musk Ox Nature Bulletin No. 740 January 25, 1964 Forest Preserve District of Cook County Seymour Simon, President David H. Thompson, Senior Naturalist THE MUSK OX Why are bones of the arctic musk ox found here in Illinois? The evidence shows that these remains date back to the Ice Age when mile- deep ice sheets covered Canada and large parts of the United States, Europe and Asia. At that time the musk ox was one of the few hardy animals that thrived along the edges of these ice sheets. Then, for thousands of years, as the climate warmed and the glaciers melted, the musk oxen followed the retreating glaciers northward. Today, they survive only on the bleak tundras of Alaska, northern Canada and the coast of Greenland . The musk ox looks somewhat like a small, unusually shaggy buffalo. It is built and upholstered for life in the most rugged climate on earth, where blizzards howl and temperatures 50 degrees below zero are common. Adult bulls weigh 500 pounds or more but appear heavier because of their thick padding of hair and wool. Cows are smaller. The dark brown to black hair -- two feet or longer on the neck, chest, sides and hind quarters -- hangs like an ankle-length skirt. The horns of both sexes are sharp, vicious weapons.

Note: This page contains sample records for the topic "greenland grenada guadeloupe" 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.


361

Camp Century survey 1986  

Science Journals Connector (OSTI)

Directional surveys of the bore-hole at Camp Century, Greenland were made in 1966, 1967 and 1969. From these surveys a surface velocity of 5.5 m/yr 3 m/yr in the direction 240 was computed. The position of the 60 metre meteorological tower near the bore-hole was measured in 1977 and 1986 with satellite navigation equipment. These measurements show a surface velocity of 3.5 m/yr 0.2 m/yr in the direction 235 2. Measurement of the surface topography in 1986 shows the bore-hole is situated on a local sloping ice divide. A differential magnetometer was used to locate the drill tower. Hand augering verified the location and showed the drill tower was buried 6.5 to 7 m beneath the 1986 snow surface, as expected from the depth-age relation. The casing was not identified. Extension of the casing to the snow surface and resurvey of the borehole will provide urgently needed information on the variation of ice flow with depth.

N.S. Gundestrup; H.B. Clausen; B.L. Hansen; J. Rand

1987-01-01T23:59:59.000Z

362

Deformation within polar ice sheets: An analysis of the Byrd Station and Camp Century borehole-tilting measurements  

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Analysis of the inclinometer surveys of the boreholes at Byrd Station, Antarctica, and Camp Century, Greenland, yields the following results. The measured strain rates at both stations, in ice deposited in the last (Wisconsin) glaciation, reduced to a standard temperature and shear stress, are only about one-third those in the Holocene ice, even though the Wisconsin ice has a strong single-maximum fabric. Variations in strain rate in the Wisconsin ice at Byrd Station are negatively correlated with the number of volcanic dust bands in the ice. It is inferred that the ice below 1800 m at Byrd Station, which has a multiple-maximum fabric, deforms much less readily than the remainder of the ice. A flow model of Nye, with index n = 3, provides a relation between shear strain rate and shear stress that fits the data from both stations satisfactorily, even though the assumption of plane strain is not strictly valid at Byrd Station. A value of flow parameter A fifteen to twenty times that given by recent data compilations and predicted by dislocation theory, has to be used for the Holocene ice. These data cover a stress range (2045 kPa) lower than in any other field experiment.

W.S.B. Paterson

1983-01-01T23:59:59.000Z

363

Comparison of 105 years of oxygen isotope and insoluble impurity profiles from the Devon Island and Camp Century ice cores  

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Oxygen-isotope profiles for the Devon Island ice cap and Camp Century Greenland are affected by a number of variables, some of which must have been the same for both sites. The two ?(18O) records spanning about 120,000 years are brought into relative alignment by comparison of major ? features, and subsequent verification that the insoluble particulate concentration records were also in phase for this alignment. The difference between the ? profiles is shown to be mainly a function of the altitude of the accumulation area for Camp Century. This altitude seems to have been higher than present for the last 100,000 years, suggesting the present flow line through the site has never been shorter. The maximum altitude for the Camp Century accumulation area is 1500 m above the present site and is almost synchronous with the maximum in particulate concentration that occurs at 16,000 yr B.P. The synchronism is likely due to the maximum sea-level lowering that exposed vast areas of continental shelf to wind erosion.

David A. Fisher

1979-01-01T23:59:59.000Z

364

1 - The Challenges of Global Warming Research  

Science Journals Connector (OSTI)

Abstract This chapter focuses on two items. First, it addresses the issue of global warming in a hostile political environment. Second, it looks at what might be called the basic research element connecting global warming to crime: research on the relationship between crime and weather. The first item addresses the nature of research itselfhow do we recognize when research is any good? There is a great deal of bad and misleading research on global warming. How do we know which is bad and which is good? The chapter begins with a discussion of three articles on Greenland melt-off, each with quite different implications, and discusses how to tell which is a legitimate research summary and which is not. It then provides a discussion of what constitutes good research generally and what one should look for when research is poorly done or intentionally misleading. For the second item, global warming and crime, we begin with a discussion of the difference between climate and weather. Much of this section is a review of Cohns work on temperature, crime, and violent crime. We also discuss the Ranson model, which provides a good description of the way in which crime can be modeled and predicted using data and research methods derived from the global warming literature.

John P. Crank; Linda S. Jacoby

2015-01-01T23:59:59.000Z

365

On the origin of Laurentia  

SciTech Connect

Laurentia, the Precambrian core of the North American continent, is surrounded by late Precambrian rift systems and therefore constitutes a suspect terrane''. A geometric and geological fit can be achieved between the Atlantic margin of Laurentia and the Pacific margin of the Gondwana craton. The enigmatic Arequipa massif along the southern Peruvian coast, that yields ca. 2.0 Ga radiometric ages, is juxtaposed with the Makkovik-Ketilidian province of the same age range in Labrador and southern Greenland. The Greenville belt continues beneath the ensialic Andes of the present day to join up with the 1.3--1.0 Ga San Ignacio and Sonsas-Aguapei orogens of the Transamazonian craton. Together with the recent identification of possible continuations of the Greenville orogen in East Antarctica and of the Taconic Appalachians in southern South America, the fit supports suggestions that Laurentia originated between East Antarctica-Australia and embryonic South America prior to the opening of the Pacific Ocean basin and amalgamation of the Gondwana Cordilleran and Appalachian margins, this implies that there may have been two supercontinents during the Neoproterozoic, before and after opening of the Pacific Ocean. As Laurentia and Gondwana appear to have collided on at least two occasions during the Paleozoic, this scenario therefore calls to question the existence of so-called supercontinental cycles. The Arica bight of the present day may reflect a primary reentrant in the South American continental margin that controlled subduction processes along the Andean margin and eventually led to uplift of the Altiplano.

Dalziel, I.W.D. (Univ. of Texas, Austin, TX (United States). Inst. for Geophysics)

1992-01-01T23:59:59.000Z

366

The microbial fate of carbon in high-latitude seas: Impact of the microbial loop on oceanic uptake of CO{sub 2}  

SciTech Connect

This dissertation examines pelagic microbial processes in high-latitude seas, how they affect regional and global carbon cycling, and how they might respond to hypothesized changes in climate. Critical to these interests is the effect of cold temperature on bacterial activity. Also important is the extent to which marine biological processes in general impact the inorganic carbon cycle. The study area is the Northeast Water (NEW) Polynya, a seasonally-recurrent opening in the permanent ice situated over the northeastern Greenland continental shelf. This work was part of an international, multi-disciplinary research project studying carbon cycling in the coastal Arctic. The first chapter describes a simple model which links a complex marine food web to a simplified ocean and atmosphere. The second chapter investigates the inorganic carbon inventory of the summertime NEW Polynya surface waters to establish the effect of biological processes on the air-sea pCO{sub 2} gradient. The third and fourth chapters use a kinetic approach to examine microbial activities in the NEW Polynya as a function of temperature and dissolved organic substrate concentration, testing the so-called Pomeroy hypothesis that microbial activity is disproportionately reduced at low environmental temperatures owing to increased organic substrate requirements. Together, the suite of data collected on microbial activities, cell size, and grazing pressure suggest how unique survival strategies adopted by an active population of high-latitude bacteria may contribute to, rather than detract from, an efficient biological carbon pump.

Yager, P.L.

1996-12-31T23:59:59.000Z

367

The new dedicated PIXE set-up at the National Environmental Research Institute, Denmark  

Science Journals Connector (OSTI)

The Niels Bohr Institute in Copenhagen was in the beginning of the 70es one of the early places for PIXE. Contributions were made to the theoretical interpretation of the PIXE spectra as well as the practical application. The home-made 4 MV van de Graaff accelerator at the Niels Bohr Institute was an excellent tool for PIXE. The accelerator which was used for many years has now found its place on a museum after more than 40 years of active service. A dedicated PIXE set-up has now been established at the National Environmental Research Institute using a new 1.7 MV Tandem Pelletron (5SDH) from NEC. The main application is elemental analysis of outdoor aerosols. The main work is unsophisticated macro analyses which do not push the equipment to its limits. This enables automated analysis of about 10 000 samples per year using very limited manpower resources. The research focuses on the contribution from various source types to the atmosphere over Europe the North Atlantic and Greenland. Source compositions and their temporal variations are studied.

Kre Kemp; Peter Waahlin

1999-01-01T23:59:59.000Z

368

Connecting Atlantic temperature variability and biological cycling in two earth system models  

Science Journals Connector (OSTI)

Abstract Connections between the interdecadal variability in North Atlantic temperatures and biological cycling have been widely hypothesized. However, it is unclear whether such connections are due to small changes in basin-averaged temperatures indicated by the Atlantic Multidecadal Oscillation (AMO) Index, or whether both biological cycling and the AMO index are causally linked to changes in the Atlantic Meridional Overturning Circulation (AMOC). We examine interdecadal variability in the annual and month-by-month diatom biomass in two Earth System Models with the same formulations of atmospheric, land, sea ice and ocean biogeochemical dynamics but different formulations of ocean physics and thus different AMOC structures and variability. In the isopycnal-layered ESM2G, strong interdecadal changes in surface salinity associated with changes in AMOC produce spatially heterogeneous variability in convection, nutrient supply and thus diatom biomass. These changes also produce changes in ice cover, shortwave absorption and temperature and hence the AMO Index. Off West Greenland, these changes are consistent with observed changes in fisheries and support climate as a causal driver. In the level-coordinate ESM2M, nutrient supply is much higher and interdecadal changes in diatom biomass are much smaller in amplitude and not strongly linked to the AMO index.

Anand Gnanadesikan; John P. Dunne; Rym Msadek

2014-01-01T23:59:59.000Z

369

Drilling deep in South Pole Ice  

E-Print Network (OSTI)

To detect the tiny flux of ultra-high energy neutrinos from active galactic nuclei or from interactions of highest energy cosmic rays with the microwave background photons needs target masses of the order of several hundred cubic kilometers. Clear Antarctic ice has been discussed as a favorable material for hybrid detection of optical, radio and acoustic signals from ultra-high energy neutrino interactions. To apply these technologies at the adequate scale hundreds of holes have to be drilled in the ice down to depths of about 2500 m to deploy the corresponding sensors. To do this on a reasonable time scale is impossible with presently available tools. Remote drilling and deployment schemes have to be developed to make such a detector design reality. After a short discussion of the status of modern hot water drilling we present here a design of an autonomous melting probe, tested 50 years ago to reach a depth of about 1000 m in Greenland ice. A scenario how to build such a probe today with modern technologies...

Karg, Timo

2014-01-01T23:59:59.000Z

370

Cadmium in arctic Alaska wildlife: Kidney and liver residues and potential exposure in indigenous people  

SciTech Connect

In arctic Alaska, cadmium (Cd) levels are of concern in kidney and liver of terrestrial and marine mammals including: bowhead whale, beluga whale, walrus, caribou, and ringed seal. Cd levels in some animals exceed threshold criteria in kidney for renal dysfunction and other effects, tolerance levels for human consumption (liver = 1 ppm, kidney = 3 ppm), and WHO weekly intake limits (500 ug Cd/week). An assessment of risk to indigenous people and to wildlife populations, will be presented. Cigarette smoking is another major source of Cd to be considered. Reports from Greenland have concluded a health risk from Cd exposure from marine dietary sources and smoking exist for these residents. Bowhead whale kidney and walrus kidney and liver represent major dietary sources of Cd (blubber and meat have very little Cd). Followed by: ringed seal liver (kidney data not available), beluga whale liver and kidney, and caribou kidney. Small portions of bowhead and walrus kidney (< 10g/week) exceed weekly intake levels. Age positively correlates with Cd levels in kidney indicating that avoiding older (larger) animals would reduce exposure. Adverse effects of Cd in wildlife were not grossly evident, however, with no historic data, it is difficult to determine if tissue concentrations are elevated. Harvest of wildlife is important to many arctic people for nutritional and cultural survival. Assessing risks associated with contaminants is essential for the wellbeing of indigenous people and wildlife. The nutritional value of the local resources and the potential inadequate alternatives must be considered.

O`Hara, T. [Department of Wildlife Management, Barrow, AK (United States); Fairbrother, A. [e, p, and t, inc., Corvallis, OR (United States); Becker, P. [Army Waterways Experiment Station, Vicksburg, MS (United States); Tarpley, R. [Texas A and M Univ., College Station, TX (United States). College of Veterinary Medicine

1995-12-31T23:59:59.000Z

371

Pre- and post-noon asymmetry in dayside auroral activity and convection related to solar wind-magnetosphere interactions  

Science Journals Connector (OSTI)

The complex chain of mechanisms involved in the transfer of solar wind energy, momentum and particles into magnetosphere-ionosphere system manifests itself in the aurora as a rich spectrum of activities. Systematic work on cusp/cleft auroral morphology, however, has provided us a rather comprehensive description of one particular class of activity. That is the poleward moving auroral forms near magnetic noon of which location and motion pattern are strongly regulated by the IMF orientation. Since it was first suggested by Sandholt in the mid-eighties, it has been an ongoing debate on whether or not this event class actually is a footprint of pulsed magnetopause reconnection. Ambiguity problems pertain mainly due to the limited longitudinal coverage of optical observations. In this paper, we will use multi-instrument data from Svalbard and Greenland to illustrate the IMF BY effect on the occurrence probability of poleward moving auroral transients on either side of noon, the IMF BY effect on the cusp location, and the relationship between moving auroral forms and excitation of polar cap flow. The data presented indicate a clear IMF BY control of cusp/cleft activities consistent with magnetopause reconnection, and time-varying magnetic reconnection appears to be an efficient driver of large-scale convection.

J. Moen; P.E. Sandholt; A. Egeland

2001-01-01T23:59:59.000Z

372

EML Surface Air Sampling Program, 1990--1993 data  

SciTech Connect

Measurements of the concentrations of specific atmospheric radionuclides in air filter samples collected for the Environmental Measurements Laboratory`s Surface Air Sampling Program (SASP) during 1990--1993, with the exception of April 1993, indicate that anthropogenic radionuclides, in both hemispheres, were at or below the lower limits of detection for the sampling and analytical techniques that were used to collect and measure them. The occasional detection of {sup 137}Cs in some air filter samples may have resulted from resuspension of previously deposited debris. Following the April 6, 1993 accident and release of radionuclides into the atmosphere at a reprocessing plant in the Tomsk-7 military nuclear complex located 16 km north of the Siberian city of Tomsk, Russia, weekly air filter samples from Barrow, Alaska; Thule, Greenland and Moosonee, Canada were selected for special analyses. The naturally occurring radioisotopes that the authors measure, {sup 7}Be and {sup 210}Pb, continue to be detected in most air filter samples. Variations in the annual mean concentrations of {sup 7}Be at many of the sites appear to result primarily from changes in the atmospheric production rate of this cosmogenic radionuclide. Short-term variations in the concentrations of {sup 7}Be and {sup 210}Pb continued to be observed at many sites at which weekly air filter samples were analyzed. The monthly gross gamma-ray activity and the monthly mean surface air concentrations of {sup 7}Be, {sup 95}Zr, {sup 137}Cs, {sup 144}Ce, and {sup 210}Pb measured at sampling sites in SASP during 1990--1993 are presented. The weekly mean surface air concentrations of {sup 7}Be, {sup 95}Zr, {sup 137}Cs, {sup 144}Ce, and {sup 210}Pb for samples collected during 1990--1993 are given for 17 sites.

Larsen, R.J.; Sanderson, C.G.; Kada, J.

1995-11-01T23:59:59.000Z

373

Multi-model Mean Nitrogen and Sulfur Deposition from the Atmospheric Chemistry and Climate Model Intercomparison Project (ACCMIP): Evaluation of Historical and Projected Future Changes  

SciTech Connect

We present multi-model global datasets of nitrogen and sulfate deposition covering time periods from 1850 to 2100, calculated within the Atmospheric Chemistry and Climate Model Intercomparison Project (ACCMIP). The computed deposition fluxes are compared to surface wet deposition and ice-core measurements. We use a new dataset of wet deposition for 2000-2002 based on critical assessment of the quality of existing regional network data. We show that for present-day (year 2000 ACCMIP time-slice), the ACCMIP results perform similarly to previously published multi-model assessments. The analysis of changes between 1980 and 2000 indicates significant differences between model and measurements over the United States, but less so over Europe. This difference points towards misrepresentation of 1980 NH3 emissions over North America. Based on ice-core records, the 1850 deposition fluxes agree well with Greenland ice cores but the change between 1850 and 2000 seems to be overestimated in the Northern Hemisphere for both nitrogen and sulfur species. Using the Representative Concentration Pathways to define the projected climate and atmospheric chemistry related emissions and concentrations, we find large regional nitrogen deposition increases in 2100 in Latin America, Africa and parts of Asia under some of the scenarios considered. Increases in South Asia are especially large, and are seen in all scenarios, with 2100 values more than double 2000 in some scenarios and reaching >1300 mgN/m2/yr averaged over regional to continental scale regions in RCP 2.6 and 8.5, ~30-50% larger than the values in any region currently (2000). Despite known issues, the new ACCMIP deposition dataset provides novel, consistent and evaluated global gridded deposition fields for use in a wide range of climate and ecological studies.

Lamarque, Jean-Francois; Dentener, Frank; McConnell, J.R.; Ro, C-U; Shaw, Mark; Vet, Robert; Bergmann, D.; Cameron-Smith, Philip; Dalsoren, S.; Doherty, R.; Faluvegi, G.; Ghan, Steven J.; Josse, B.; Lee, Y. H.; MacKenzie, I. A.; Plummer, David; Shindell, Drew; Skeie, R. B.; Stevenson, D. S.; Strode, S.; Zeng, G.; Curran, M.; Dahl-Jensen, D.; Das, S.; Fritzsche, D.; Nolan, M.

2013-08-20T23:59:59.000Z

374

Development of Exhibit on Arctic Climate Change Called The Arctic: A Friend Acting Strangely Exhibition  

SciTech Connect

The exhibition, The Arctic: A Friend Acting Strangely, was developed at the Smithsonian Institutions National Museum of Natural History (NMNH) as a part of the museums Forces of Change exhibit series on global change. It opened to the public in Spring 2006, in conjunction with another Forces of Change exhibit on the Earths atmosphere called Change Is in the Air. The exhibit was a 2000 square-foot presentation that explored the forces and consequences of the changing Arctic as documented by scientists and native residents alike. Native peoples of the Arctic have always lived with year-to-year fluctuations in weather and ice conditions. In recent decades, they have witnessed that the climate has become unpredictable, the land and sea unfamiliar. An elder in Arctic Canada recently described the weather as uggianaqtuq an Inuit word that can suggest strange, unexpected behavior, sometimes described as that of a friend acting strangely. Scientists too have been documenting dramatic changes in the Arctic. Air temperatures have warmed over mostthough not allof the Arctic since the 1950s; Arctic precipitation may have increased by as much as 8%; seasonal melting of the Greenland Ice Sheet has increased on average by 16% since 1979; polar-orbiting satellites have measured a 1520% decline in sea ice extent since the 1970s; aircraft reconnaissance and ship observations show a steady decrease in sea ice since the 1950s. In response to this warming, plant distributions have begun to shift and animals are changing their migration routes. Some of these changes may have beneficial effects while others may bring hardship or have costly implications. And, many scientists consider arctic change to be a bell-weather for large-scale changes in other regions of the world. The exhibition included text, photos artifacts, hands-on interactives and other exhibitry that illustrated the changes being documented by indigenous people and scientists alike.

Stauffer, Barbara W.

2006-04-01T23:59:59.000Z

375

Evaluation of Preindustrial to Present-day Black Carbon and its Albedo Forcing from Atmospheric Chemistry and Climate Model Intercomparison Project (ACCMIP)  

SciTech Connect

As a part of the Atmospheric Chemistry and Climate Model Intercomparison Project (ACCMIP), we evaluate the historical black carbon (BC) aerosols simulated by 8 ACCMIP models against the observations including 12 ice core records, a long-term surface mass concentrations and recent Arctic BC snowpack measurements. We also estimate BC albedo forcing by performing additional simulations using the NCAR Community Land and Sea-Ice model 4 with prescribed meteorology from 1996-2000, which includes the SNICAR BC-snow model. We evaluated the vertical profile of BC snow concentrations from these offline simulations to using recent BC snowpack measurements. Despite using the same BC emissions, global BC burden differs by approximately a factor of 3 among models due to the differences in aerosol removal parameterizations and simulated meteorology among models; 34 Gg to 103 Gg in 1850 and 82 Gg to 315 Gg in 2000. However,models agree well on 2.5~3 times increase in the global BC burden from preindustrial to present-day, which matches with the 2.5 times increase in BC emissions. We find a large model diversity at both NH and SH high latitude regions for BC burden and at SH high latitude regions for deposition fluxes. The ACCMIP simulations match the observed BC mass concentrations well in Europe and North America except at Jungfrauch and Ispra. However, the models fail to capture the Arctic BC seasonality due tosevere underestimations during winter and spring. Compared to recent snowpack measurements, the simulated vertically resolved BC snow concentrations are, on average, within a factor of 2-3 of observations except for Greenland and Arctic Ocean. However, model and observation differ widely due to missing interannual variations in emissions and possibly due to the choice of the prescribed meteorology period (i.e., 1996-2000).

Lee, Y. H.; Lamarque, J.-F.; Flanner, M. G.; Jiao, C.; Shindell, Drew; Berntsen, T.; Bisiauxs, M.; Cao, J.; Collins, W. J.; Curran, M.; Edwards, R.; Faluvegi, G.; Ghan, Steven J.; Horowitz, L.; McConnell, J.R.; Ming, J.; Myhre, G.; Nagashima, T.; Naik, Vaishali; Rumbold, S.; Skeie, R. B.; Sudo, K.; Takemura, T.; Thevenon, F.; Xu, B.; Yoon, Jin-Ho

2013-03-05T23:59:59.000Z

376

Atlantic Ocean CARINA data: overview and salinity adjustments  

SciTech Connect

Water column data of carbon and carbon-relevant hydrographic and hydrochemical parameters from 188 previously non-publicly available cruise data sets in the Arctic Mediterranean Seas, Atlantic and Southern Ocean have been retrieved and merged into a new database: CARINA (CARbon dioxide IN the Atlantic Ocean). The data have gone through rigorous quality control procedures to assure the highest possible quality and consistency. The data for the pertinent parameters in the CARINA database were objectively examined in order to quantify systematic differences in the reported values, i.e. secondary quality control. Systematic biases found in the data have been corrected in the three data products: merged data files with measured, calculated and interpolated data for each of the three CARINA regions, i.e. the Arctic Mediterranean Seas, the Atlantic and the Southern Ocean. These products have been corrected to be internally consistent. Ninety-eight of the cruises in the CARINA database were conducted in the Atlantic Ocean, defined here as the region south of the Greenland-Iceland-Scotland Ridge and north of about 30 S. Here we present an overview of the Atlantic Ocean synthesis of the CARINA data and the adjustments that were applied to the data product. We also report the details of the secondary QC (Quality Control) for salinity for this data set. Procedures of quality control including crossover analysis between stations and inversion analysis of all crossover data are briefly described. Adjustments to salinity measurements were applied to the data from 10 cruises in the Atlantic Ocean region. Based on our analysis we estimate the internal consistency of the CARINA-ATL salinity data to be 4.1 ppm. With these adjustments the CARINA data products are consistent both internally was well as with GLODAP data, an oceanographic data set based on the World Hydrographic Program in the 1990s, and is now suitable for accurate assessments of, for example, oceanic carbon inventories and uptake rates and for model validation.

Tanhua, T. [IFM-GEOMAR, Leibniz Institute for Marine Sciences, Chemical Oceanography, Kiel, Germany; Steinfeldt, R. [University of Bremen, Bremen, Germany; Key, Robert [Princeton University; Brown, P. [University of East Anglia, Norwich, United Kingdom; Gruber, N. [ETH Zurich, Switzerland; Wanninkhof, R. [Atlantic Oceanographic & Meteorological Laboratory, NOAA; Perez, F.F. [Instituto de Investigaciones Marinas de Vigo, CSIC, Vigo, Spain; Kortzinger, A. [IFM-GEOMAR, Leibniz Institute for Marine Sciences, Chemical Oceanography, Kiel, Germany; Velo, A. [Instituto de Investigaciones Marinas de Vigo, CSIC, Vigo, Spain; Schuster, U. [University of East Anglia, Norwich, United Kingdom; Van Heuven, S. [University of Groningen, The Netherlands; Bullister, J.L. [NOAA Pacific Marine Environmental Laboratory; Stendardo, I. [ETH Zurich, Switzerland; Hoppema, M. [Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany; Olsen, Are [Bjerknes Centre for Climate Research, UNIFOB AS, Bergen, Norway; Kozyr, Alexander [ORNL; Pierrot, D. [Cooperative Institute of Marine and Atmospheric Sciences, U. Miami; Schirnick, C. [IFM-GEOMAR, Leibniz Institute for Marine Sciences, Chemical Oceanography, Kiel, Germany; Wallace, D.W.R. [IFM-GEOMAR, Leibniz Institute for Marine Sciences, Chemical Oceanography, Kiel, Germany

2010-01-01T23:59:59.000Z

377

A multi-resolution method for climate system modeling: application of spherical centroidal Voronoi tessellations  

SciTech Connect

During the next decade and beyond, climate system models will be challenged to resolve scales and processes that are far beyond their current scope. Each climate system component has its prototypical example of an unresolved process that may strongly influence the global climate system, ranging from eddy activity within ocean models, to ice streams within ice sheet models, to surface hydrological processes within land system models, to cloud processes within atmosphere models. These new demands will almost certainly result in the develop of multiresolution schemes that are able, at least regionally, to faithfully simulate these fine-scale processes. Spherical centroidal Voronoi tessellations (SCVTs) offer one potential path toward the development of a robust, multiresolution climate system model components. SCVTs allow for the generation of high quality Voronoi diagrams and Delaunay triangulations through the use of an intuitive, user-defined density function. In each of the examples provided, this method results in high-quality meshes where the quality measures are guaranteed to improve as the number of nodes is increased. Real-world examples are developed for the Greenland ice sheet and the North Atlantic ocean. Idealized examples are developed for oceanice shelf interaction and for regional atmospheric modeling. In addition to defining, developing, and exhibiting SCVTs, we pair this mesh generation technique with a previously developed finite-volume method. Our numerical example is based on the nonlinear, shallow water equations spanning the entire surface of the sphere. This example is used to elucidate both the potential benefits of this multiresolution method and the challenges ahead.

Ringler, Todd [Los Alamos National Laboratory; Ju, Lili [University of South Carolina; Gunzburger, Max [Florida State University

2008-01-01T23:59:59.000Z

378

Miljoforden Website | Open Energy Information  

Open Energy Info (EERE)

Miljoforden Website Miljoforden Website Jump to: navigation, search Tool Summary LAUNCH TOOL Name: Miljoforden Website Focus Area: Natural Gas Topics: Deployment Data Website: www.miljofordon.se/in-english/this-is-miljofordon-se Equivalent URI: cleanenergysolutions.org/content/miljoforden-website Language: "English,Swedish" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Provençal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volapük, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.

379

Overview of China's Vehicle Emission Control Program: Past Successes and  

Open Energy Info (EERE)

Overview of China's Vehicle Emission Control Program: Past Successes and Overview of China's Vehicle Emission Control Program: Past Successes and Future Prospects Jump to: navigation, search Tool Summary LAUNCH TOOL Name: Overview of China's Vehicle Emission Control Program: Past Successes and Future Prospects Focus Area: Propane Topics: Socio-Economic Website: theicct.org/sites/default/files/publications/Retrosp_final_bilingual.p Equivalent URI: cleanenergysolutions.org/content/overview-china's-vehicle-emission-con Language: "English,Chinese" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Provençal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volapük, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.

380

Photovoltaics Design and Installation Manual | Open Energy Information  

Open Energy Info (EERE)

Photovoltaics Design and Installation Manual Photovoltaics Design and Installation Manual Jump to: navigation, search Tool Summary LAUNCH TOOL Name: Photovoltaics Design and Installation Manual Agency/Company /Organization: Solar Energy International Sector: Energy Focus Area: Renewable Energy, Solar, - Solar PV Resource Type: Training materials User Interface: Other Website: www.solarenergy.org/bookstore/photovoltaics-design-installation-manual Cost: Paid Language: "English, Spanish; Castilian" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Provençal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volapük, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.

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381

OLADE-Solar Thermal World Portal | Open Energy Information  

Open Energy Info (EERE)

form form View source History View New Pages Recent Changes All Special Pages Semantic Search/Querying Get Involved Help Apps Datasets Community Login | Sign Up Search Page Edit with form History Facebook icon Twitter icon » OLADE-Solar Thermal World Portal Jump to: navigation, search Tool Summary Name: OLADE-Solar Thermal World Portal Agency/Company /Organization: Latin American Energy Organization (OLADE) Sector: Energy Focus Area: Renewable Energy, Solar, - Concentrating Solar Power, - Solar Hot Water User Interface: Website Website: www.solarthermalworld.org/ Cost: Free UN Region: Caribbean, South America Language: "English, Spanish; Castilian" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Proven√ßal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volap√ºk, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.

382

Freight Best Practice Website | Open Energy Information  

Open Energy Info (EERE)

Freight Best Practice Website Freight Best Practice Website Jump to: navigation, search Tool Summary LAUNCH TOOL Name: Freight Best Practice Website Focus Area: Public Transit Topics: Policy, Deployment, & Program Impact Website: www.freightbestpractice.org.uk/ Equivalent URI: cleanenergysolutions.org/content/freight-best-practice-website Language: "English,Welsh" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Provençal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volapük, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.

383

COMFAR III: Computer Model for Feasibility Analysis and Reporting | Open  

Open Energy Info (EERE)

COMFAR III: Computer Model for Feasibility Analysis and Reporting COMFAR III: Computer Model for Feasibility Analysis and Reporting Jump to: navigation, search Tool Summary Name: COMFAR III: Computer Model for Feasibility Analysis and Reporting Agency/Company /Organization: United Nations Industrial Development Organization Focus Area: Industry Resource Type: Software/modeling tools User Interface: Desktop Application Website: www.unido.org/index.php?id=o3470 Language: "Arabic, Chinese, English, French, German, Japanese, Portuguese, Russian, Spanish; Castilian" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Provençal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volapük, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.

384

Sustainable Logistics Website | Open Energy Information  

Open Energy Info (EERE)

Sustainable Logistics Website Sustainable Logistics Website Jump to: navigation, search Tool Summary LAUNCH TOOL Name: Sustainable Logistics Website Focus Area: Clean Transportation Topics: Best Practices Website: www.duurzamelogistiek.nl/ Equivalent URI: cleanenergysolutions.org/content/sustainable-logistics-website Language: "English,Dutch" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Provençal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volapük, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.

385

Canadian National Energy Use Database: Statistics and Analysis | Open  

Open Energy Info (EERE)

Canadian National Energy Use Database: Statistics and Analysis Canadian National Energy Use Database: Statistics and Analysis Jump to: navigation, search Tool Summary LAUNCH TOOL Name: Canadian National Energy Use Database: Statistics and Analysis Focus Area: Energy Efficiency Topics: Potentials & Scenarios Website: oee.nrcan.gc.ca/corporate/statistics/neud/dpa/home.cfm?attr=24 Equivalent URI: cleanenergysolutions.org/content/canadian-national-energy-use-database Language: "English,French" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Provençal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volapük, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.

386

Improved Biomass Cooking Stoves | Open Energy Information  

Open Energy Info (EERE)

Improved Biomass Cooking Stoves Improved Biomass Cooking Stoves Jump to: navigation, search Tool Summary LAUNCH TOOL Name: Improved Biomass Cooking Stoves Agency/Company /Organization: various Sector: Energy Focus Area: Biomass Phase: Determine Baseline, Evaluate Options, Prepare a Plan, Create Early Successes Topics: Co-benefits assessment, - Energy Access Resource Type: Case studies/examples, Guide/manual, Presentation, Video User Interface: Website Website: ttp://www.bioenergylists.org/ Cost: Free Language: "English, Spanish; Castilian" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Provençal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volapük, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.

387

Handbook of Emission Factors for Road Transport (HBEFA) | Open Energy  

Open Energy Info (EERE)

of Emission Factors for Road Transport (HBEFA) of Emission Factors for Road Transport (HBEFA) Jump to: navigation, search Tool Summary LAUNCH TOOL Name: Handbook of Emission Factors for Road Transport (HBEFA) Focus Area: Clean Transportation Topics: Policy, Deployment, & Program Impact Website: www.hbefa.net/e/index.html Equivalent URI: cleanenergysolutions.org/content/handbook-emission-factors-road-transp Language: "English,French,German" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Provençal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volapük, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.

388

Renewable Energy and Energy Efficiency Toolkit Website | Open Energy  

Open Energy Info (EERE)

Renewable Energy and Energy Efficiency Toolkit Website Renewable Energy and Energy Efficiency Toolkit Website Jump to: navigation, search Tool Summary LAUNCH TOOL Name: Renewable Energy and Energy Efficiency Toolkit Website Focus Area: Renewable Energy Topics: Policy Impacts Website: toolkits.reeep.org/ Equivalent URI: cleanenergysolutions.org/content/renewable-energy-and-energy-efficienc Language: "English,Chinese,French,Portuguese,Spanish" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Provençal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volapük, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.

389

IGES-Market Mechanism Group | Open Energy Information  

Open Energy Info (EERE)

IGES-Market Mechanism Group IGES-Market Mechanism Group Jump to: navigation, search Tool Summary LAUNCH TOOL Name: IGES-Market Mechanism Agency/Company /Organization: Institute for Global Environmental Strategies (IGES) Sector: Climate, Energy Focus Area: Renewable Energy Topics: Market analysis Resource Type: Training materials Website: www.iges.or.jp/en/cdm/index.html Cost: Free Language: "English, Japanese" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Provençal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volapük, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.

390

Eco TransIT World | Open Energy Information  

Open Energy Info (EERE)

Eco TransIT World Eco TransIT World Jump to: navigation, search Tool Summary LAUNCH TOOL Name: Eco TransIT World Focus Area: Low Carbon Communities Topics: Opportunity Assessment & Screening Website: www.ecotransit.org/index.en.html Equivalent URI: cleanenergysolutions.org/content/eco-transit-world Language: "English,Dutch,French,German,Spanish" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Provençal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volapük, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.

391

CRiSTAL Project Management Tool | Open Energy Information  

Open Energy Info (EERE)

CRiSTAL Project Management Tool CRiSTAL Project Management Tool Jump to: navigation, search Tool Summary Name: CRiSTAL Project Management Tool Agency/Company /Organization: International Institute for Sustainable Development (IISD) Sector: Climate, Energy, Land Topics: Implementation Resource Type: Guide/manual, Software/modeling tools User Interface: Spreadsheet Website: www.iisd.org/cristaltool/ Cost: Free Language: "English, French, Portuguese, Spanish; Castilian" is not in the list of possible values (Abkhazian, Achinese, Acoli, Adangme, Adyghe; Adygei, Afar, Afrihili, Afrikaans, Afro-Asiatic languages, Ainu, Akan, Akkadian, Albanian, Aleut, Algonquian languages, Altaic languages, Amharic, Angika, Apache languages, Arabic, Aragonese, Arapaho, Arawak, Armenian, Aromanian; Arumanian; Macedo-Romanian, Artificial languages, Assamese, Asturian; Bable; Leonese; Asturleonese, Athapascan languages, Australian languages, Austronesian languages, Avaric, Avestan, Awadhi, Aymara, Azerbaijani, Balinese, Baltic languages, Baluchi, Bambara, Bamileke languages, Banda languages, Bantu (Other), Basa, Bashkir, Basque, Batak languages, Beja; Bedawiyet, Belarusian, Bemba, Bengali, Berber languages, Bhojpuri, Bihari languages, Bikol, Bini; Edo, Bislama, Blin; Bilin, Blissymbols; Blissymbolics; Bliss, Bosnian, Braj, Breton, Buginese, Bulgarian, Buriat, Burmese, Caddo, Catalan; Valencian, Caucasian languages, Cebuano, Celtic languages, Central American Indian languages, Central Khmer, Chagatai, Chamic languages, Chamorro, Chechen, Cherokee, Cheyenne, Chibcha, Chichewa; Chewa; Nyanja, Chinese, Chinook jargon, Chipewyan; Dene Suline, Choctaw, Chuukese, Chuvash, Classical Newari; Old Newari; Classical Nepal Bhasa, Classical Syriac, Coptic, Cornish, Corsican, Cree, Creek, Creoles and pidgins , Crimean Tatar; Crimean Turkish, Croatian, Cushitic languages, Czech, Dakota, Danish, Dargwa, Delaware, Dinka, Divehi; Dhivehi; Maldivian, Dogri, Dogrib, Dravidian languages, Duala, Dutch; Flemish, Dyula, Dzongkha, Eastern Frisian, Efik, Egyptian (Ancient), Ekajuk, Elamite, English, Erzya, Esperanto, Estonian, Ewe, Ewondo, Fang, Fanti, Faroese, Fijian, Filipino; Pilipino, Finnish, Finno-Ugrian languages, Fon, French, Friulian, Fulah, Ga, Gaelic; Scottish Gaelic, Galibi Carib, Galician, Ganda, Gayo, Gbaya, Geez, Georgian, German, Germanic languages, Gilbertese, Gondi, Gorontalo, Gothic, Grebo, Greek, Modern, Guarani, Gujarati, Gwich'in, Haida, Haitian; Haitian Creole, Hausa, Hawaiian, Hebrew, Herero, Hiligaynon, Himachali languages; Western Pahari languages, Hindi, Hiri Motu, Hittite, Hmong; Mong, Hungarian, Hupa, Iban, Icelandic, Ido, Igbo, Ijo languages, Iloko, Inari Sami, Indic languages, Indo-European languages, Indonesian, Ingush, Interlingue; Occidental, Inuktitut, Inupiaq, Iranian languages, Irish, Iroquoian languages, Italian, Japanese, Javanese, Judeo-Arabic, Judeo-Persian, Kabardian, Kabyle, Kachin; Jingpho, Kalaallisut; Greenlandic, Kalmyk; Oirat, Kamba, Kannada, Kanuri, Kara-Kalpak, Karachay-Balkar, Karelian, Karen languages, Kashmiri, Kashubian, Kawi, Kazakh, Khasi, Khoisan languages, Khotanese; Sakan, Kikuyu; Gikuyu, Kimbundu, Kinyarwanda, Kirghiz; Kyrgyz, Klingon; tlhIngan-Hol, Komi, Kongo, Konkani, Korean, Kosraean, Kpelle, Kru languages, Kuanyama; Kwanyama, Kumyk, Kurdish, Kurukh, Kutenai, Ladino, Lahnda, Lamba, Land Dayak languages, Lao, Latin, Latvian, Lezghian, Limburgan; Limburger; Limburgish, Lingala, Lithuanian, Lojban, Lower Sorbian, Lozi, Luba-Katanga, Luba-Lulua, Luiseno, Lule Sami, Lunda, Luo (Kenya and Tanzania), Lushai, Luxembourgish; Letzeburgesch, Macedonian, Madurese, Magahi, Maithili, Makasar, Malagasy, Malay, Malayalam, Maltese, Manchu, Mandar, Mandingo, Manipuri, Manobo languages, Manx, Maori, Mapudungun; Mapuche, Marathi, Mari, Marshallese, Marwari, Masai, Mayan languages, Mende, Mi'kmaq; Micmac, Minangkabau, Mirandese, Mohawk, Moksha, Mon-Khmer languages, Mongo, Mongolian, Mossi, Multiple languages, Munda languages, N'Ko, Nahuatl languages, Nauru, Navajo; Navaho, Ndebele, North; North Ndebele, Ndebele, South; South Ndebele, Ndonga, Neapolitan, Nepal Bhasa; Newari, Nepali, Nias, Niger-Kordofanian languages, Nilo-Saharan languages, Niuean, North American Indian languages, Northern Frisian, Northern Sami, Norwegian, Nubian languages, Nyamwezi, Nyankole, Nyoro, Nzima, Occitan (post 1500); Provençal, Ojibwa, Oriya, Oromo, Osage, Ossetian; Ossetic, Otomian languages, Pahlavi, Palauan, Pali, Pampanga; Kapampangan, Pangasinan, Panjabi; Punjabi, Papiamento, Papuan languages, Pedi; Sepedi; Northern Sotho, Persian, Philippine languages, Phoenician, Pohnpeian, Polish, Portuguese, Prakrit languages, Pushto; Pashto, Quechua, Rajasthani, Rapanui, Rarotongan; Cook Islands Maori, Romance languages, Romanian; Moldavian; Moldovan, Romansh, Romany, Rundi, Russian, Salishan languages, Samaritan Aramaic, Sami languages, Samoan, Sandawe, Sango, Sanskrit, Santali, Sardinian, Sasak, Scots, Selkup, Semitic languages, Serbian, Serer, Shan, Shona, Sichuan Yi; Nuosu, Sicilian, Sidamo, Sign Languages, Siksika, Sindhi, Sinhala; Sinhalese, Sino-Tibetan languages, Siouan languages, Skolt Sami, Slave (Athapascan), Slavic languages, Slovak, Slovenian, Sogdian, Somali, Songhai languages, Soninke, Sorbian languages, Sotho, Southern, South American Indian (Other), Southern Altai, Southern Sami, Spanish; Castilian, Sranan Tongo, Sukuma, Sumerian, Sundanese, Susu, Swahili, Swati, Swedish, Swiss German; Alemannic; Alsatian, Syriac, Tagalog, Tahitian, Tai languages, Tajik, Tamashek, Tamil, Tatar, Telugu, Tereno, Tetum, Thai, Tibetan, Tigre, Tigrinya, Timne, Tiv, Tlingit, Tok Pisin, Tokelau, Tonga (Nyasa), Tonga (Tonga Islands), Tsimshian, Tsonga, Tswana, Tumbuka, Tupi languages, Turkish, Turkmen, Tuvalu, Tuvinian, Twi, Udmurt, Ugaritic, Uighur; Uyghur, Ukrainian, Umbundu, Uncoded languages, Undetermined, Upper Sorbian, Urdu, Uzbek, Vai, Venda, Vietnamese, Volapük, Votic, Wakashan languages, Walamo, Walloon, Waray, Washo, Welsh, Western Frisian, Wolof, Xhosa, Yakut, Yao, Yapese, Yiddish, Yoruba, Yupik languages, Zande languages, Zapotec, Zaza; Dimili; Dimli; Kirdki; Kirmanjki; Zazaki, Zenaga, Zhuang; Chuang, Zulu, Zuni) for this property.