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Note: This page contains sample records for the topic "greenland ice sheet" 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.


1

Complex systems influence melting of Greenland ice sheet  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Complex systems influence melting of Greenland ice sheet Complex systems influence melting of Greenland ice sheet International research team's field work shows that, well, things...

2

Home Atmosphere Sea Ice Ocean Land Greenland Biology Greenland Ice Sheet Mass Balance  

E-Print Network [OSTI]

Home Atmosphere Sea Ice Ocean Land Greenland Biology Greenland Ice Sheet Mass Balance E. Hanna 1 ice loss over Greenland. Recent warm events are about the same magnitude, if not smaller, than those warming, remain incompletely understood. Satellite Observations The Greenland ice sheet (GrIS) contains 7

Box, Jason E.

3

Coherent radar ice thickness measurements over the Greenland ice sheet  

E-Print Network [OSTI]

We developed two 150-MHz coherent radar depth sounders for ice thickness measurements over the Greenland ice sheet. We developed one of these using connectorized components and the other using radio frequency integrated circuits (RFICs). Both...

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

4

THE CONTRIBUTION OF GREENLAND ICE SHEET MELTING TO  

E-Print Network [OSTI]

THE CONTRIBUTION OF GREENLAND ICE SHEET MELTING TO GLOBAL SEA-LEVEL CHANGE Conor Mc three major sources, the Greenland ice sheet, Antarctica, and other eustatic components. Each has its own predictable spatial signal, and particular attention was paid to the Greenland ice sheet, given

5

Azimuth Variation in Microwave Backscatter over the Greenland Ice Sheet  

E-Print Network [OSTI]

Azimuth Variation in Microwave Backscatter over the Greenland Ice Sheet Ivan S. Ashcraft and David backscatter measurements are becoming an important tool for monitoring the dynamic behavior of the Greenland ice sheet. However, most Greenland studies assume constant backscatter for varying azimuth angles

Long, David G.

6

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

Broader source: All U.S. Department of Energy (DOE) Office Webpages (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...

7

Greenland Ice Sheet Retreat Since the Little Ice Age  

E-Print Network [OSTI]

and I. Willis (2012), Greenland's shrinking ice cover: "fastfluctuations in southeast Greenland, Nat. Geosci. , 5(6),T. Decker (2011), Analysis of Greenland marine- terminating

Beitch, Marci Jillian

2014-01-01T23:59:59.000Z

8

white paper, 9 March 2009 An ice core to reconstruct Greenland ice sheet mass balance  

E-Print Network [OSTI]

white paper, 9 March 2009 1 An ice core to reconstruct Greenland a handful of years suggest a profound Greenland ice sheet mass balance sensitivity (2000) found that the Greenland ice sheet lost as much as 2/3 its current

Box, Jason E.

9

Ice sheets  

E-Print Network [OSTI]

is eroding West Antarctic Ice Sheet. Geophysical Researchand Yungel, J. (2000). Greenland Ice Sheet: High-Elevation2004). The west Antarctic ice sheet and long term climate

Bentley, Charles G.; Thomas, Robert H.; Velicogna, Isabella

2007-01-01T23:59:59.000Z

10

Hydrological and biogeochemical cycling along the Greenland ice sheet margin  

E-Print Network [OSTI]

Global warming has led to a significant increase in Greenland ice sheet (GrIS) melt and runoff since 1990, resulting in escalated export of fresh water and associated sediment to the surrounding North Atlantic and Arctic ...

Bhatia, Maya Pilar, 1979-

2012-01-01T23:59:59.000Z

11

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

12

Determining Greenland Ice Sheet sensitivity to regional climate change: one-way coupling of a 3-D thermo-mechanical ice sheet model with a mesoscale climate model  

E-Print Network [OSTI]

in running RCMs over Greenland to produce high-qualityoutlet glaciers. For Greenland, this detail is specificallyCurrently, no coupled Greenland Ice Sheet model experiment

Schlegel, Nicole-Jeanne

2011-01-01T23:59:59.000Z

13

Update of Greenland Ice Sheet Mass Loss: Exponential? 26 December 2012  

E-Print Network [OSTI]

1 Update of Greenland Ice Sheet Mass Loss: Exponential? 26 December 2012 James Hansen and Makiko Sato Shepherd et al. (2012) provide an update of the mass loss by the Greenland ice sheet (and at the data seems warranted. A crucial question is how rapidly the Greenland (or Antarctic) ice sheet can

Hansen, James E.

14

Greenland Ice Sheet Surface Air Temperature Variability: 18402007* JASON E. BOX  

E-Print Network [OSTI]

Greenland Ice Sheet Surface Air Temperature Variability: 18402007* JASON E. BOX Byrd Polar, seasonal, and annual mean Greenland ice sheet near- surface air temperatures. Independent observations Greenland in autumn and southern Greenland in winter. Spring trends marked the 1920s warming onset, while

Howat, Ian M.

15

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.

16

Impact of Greenland and Antarctic ice sheet interactions on climate sensitivity  

E-Print Network [OSTI]

Impact of Greenland and Antarctic ice sheet interactions on climate sensitivity H. Goelzer P versions including interactive Greenland and Ant- arctic ice sheet models and model versions with fixed ice a few global climate models exist that include dynami- cally coupled models for the Greenland (e

Goelzer, Heiko

17

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.

18

Ocean Challenge, Vol.19, Autumn 2012 Early Online The shrinking Greenland ice Sheet  

E-Print Network [OSTI]

Ocean Challenge, Vol.19, Autumn 2012 Early Online The shrinking Greenland ice Sheet The Greenland and south-east- ern Greenland. Higher ocean temperatures are thought to have played a role. However, the circulation within Greenland's fjords is not well known, and the interaction between glacial ice and the ocean

Johnson, Helen

19

Relating Microwave Backscatter Azimuth Modulation to Surface Properties of the Greenland Ice Sheet  

E-Print Network [OSTI]

Relating Microwave Backscatter Azimuth Modulation to Surface Properties of the Greenland Ice Sheet modulation of the normalized radar cross- section in satellite data sets over Greenland is investigated. Data sastrugi are estimated. I. INTRODUCTION The Greenland ice sheet is a critical area of study in esti- mating

Long, David G.

20

Earliest Holocene south Greenland ice sheet retreat within its late Holocene extent  

E-Print Network [OSTI]

Earliest Holocene south Greenland ice sheet retreat within its late Holocene extent Anders E, British Columbia, Canada Abstract Early Holocene summer warmth drove dramatic Greenland ice sheet (GIS Greenland, significantly earlier than previous estimates, and 6.8 0.1 ka to 7.9 0.1 ka in southwest

Note: This page contains sample records for the topic "greenland ice sheet" 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

Radar Measurements of Ice Sheet Thickness of Outlet Glaciers in Greenland D. Braaten+  

E-Print Network [OSTI]

Radar Measurements of Ice Sheet Thickness of Outlet Glaciers in Greenland D. Braaten+ and S of Kansas Lawrence, KS 66045 U.S.A. Abstract We have conducted airborne measurements over the Greenland the mass balance of the Greenland ice sheet, the University of Kansas has been operating an airborne radio

Kansas, University of

22

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 microwave methods. The method should be useful for long-term monitoring of the melt area of the Greenland of MODIS retrievals of the western portion of the Greenland ice sheet over the period 2000 to 2006

Dozier, Jeff

23

Geoid displacement about Greenland resulting from past and present-day mass changes in the Greenland Ice Sheet  

E-Print Network [OSTI]

Geoid displacement about Greenland resulting from past and present- day mass changes in the Greenland Ice Sheet K. Fleming, Z. Martinec, and J. Hagedoorn Geodesy and Remote Sensing, Geo-isostatic adjustment (GIA) following the Last Glacial Maximum and from present- day mass changes in the Greenland Ice

Cerveny, Vlastislav

24

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.

25

Analysis of the Greenland ice sheet loss from remote sensing data*  

E-Print Network [OSTI]

Analysis of the Greenland ice sheet loss from remote sensing data* Peter Limkilde Svendsen, Allan corresponding to the missing data removed. 2950 730.5 365.25 183 122 50 40 30 20 0 0.05 0.1 0.15 Greenland frequency content, amplitude spectrum Period [d] Amplitude[m] Greenland mean Greenland maximum Figure 1: EWH

26

Net accumulation of the Greenland ice sheet: High resolution modeling of climate changes  

E-Print Network [OSTI]

: Kiilsholm, S., J. H. Christensen, K. Dethloff, and A. Rinke, Net accumulation of the Greenland ice sheetNet accumulation of the Greenland ice sheet: High resolution modeling of climate changes Sissi, Denmark Klaus Dethloff and Annette Rinke Alfred Wegener Institute for Polar and Marine Research

Born, Andreas

27

Response of the Greenland and Antarctic Ice Sheets to Multi-Millennial Greenhouse Warming in the Earth  

E-Print Network [OSTI]

Response of the Greenland and Antarctic Ice Sheets to Multi-Millennial Greenhouse Warming of the Greenland and Antarctic ice sheets to sustained multi-millennial greenhouse warming. Use was made of fully polar regions. This leads to an almost complete disintegration of the Greenland ice sheet after 3

Goelzer, Heiko

28

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.

29

Acceleration of the Greenland ice sheet mass loss as observed by GRACE: Confidence and sensitivity  

E-Print Network [OSTI]

Acceleration of the Greenland ice sheet mass loss as observed by GRACE: Confidence and sensitivity: Greenland mass loss acceleration confidence intervals GRACE a b s t r a c t We examine the scale and spatial distribution of the mass change acceleration in Greenland and its statistical significance, using processed

30

A spatially calibrated model of annual accumulation rate on the Greenland Ice Sheet (19582007)  

E-Print Network [OSTI]

on the Greenland Ice Sheet (19582007) Evan W. Burgess,1 Richard R. Forster,1 Jason E. Box,2,3 Ellen Mosley 10 September 2009; accepted 21 October 2009; published 10 April 2010. [1] Past estimates of Greenland patterns, which are modeled via spatial interpolation of root mean squared errors. Mean 19582007 Greenland

Howat, Ian M.

31

Modelling Lake Volumes and Runoff on the Western Greenland Ice Sheet  

E-Print Network [OSTI]

Supra-glacial lakes can act as a key regulator of variable surface meltwater to the ice-bed interface on the Greenland Ice Sheet. In light of recent numerical studies focussing on the impact of variable surface meltwater inputs to ice sheet dynamics...

Lund, Sarah

32

07/06/2009 Melting Ice Could Lead to Massive Waves of Climate Refugees Treehugger 06/30/2009 MELTING GREENLAND ICE SHEETS MAY THREATEN  

E-Print Network [OSTI]

/30/2009 MELTING GREENLAND ICE SHEETS MAY THREATEN NORTHEAST U.S., CANADA Federal News Service 06/30/2009 Sea raises spectre of displaced humanity peopleandplanet.net 06/16/2009 Melting Greenland Ice Sheets May Report - Online 06/02/2009 Melting Greenland Ice Sheets May Threaten Northeast, Canada usagnet 06

Hu, Aixue

33

Probabilistic calibration of a Greenland Ice Sheet model using spatially-resolved synthetic observations: toward projections of ice mass loss with uncertainties  

E-Print Network [OSTI]

1 Probabilistic calibration of a Greenland Ice Sheet model using spatially-resolved synthetic on how well the model reproduces the Greenland Ice Sheet profile. We improve on the previous state et al., 2012). Here, we focus on the Greenland Ice Sheet component of future sea level rise

Haran, Murali

34

Decay of the Greenland Ice Sheet due to surface-meltwater-induced acceleration of basal sliding  

E-Print Network [OSTI]

Simulations of the Greenland Ice Sheet are carried out with a high-resolution version of the ice-sheet model SICOPOLIS for several global-warming scenarios for the period 1990-2350. In particular, the impact of surface-meltwater-induced acceleration of basal sliding on the stability of the ice sheet is investigated. A parameterization for the acceleration effect is developed for which modelled and measured mass losses of the ice sheet in the early 21st century agree well. The main findings of the simulations are: (i) the ice sheet is generally very susceptible to global warming on time-scales of centuries, (ii) surface-meltwater-induced acceleration of basal sliding leads to a pronounced speed-up of ice streams and outlet glaciers, and (iii) this ice-dynamical effect accelerates the decay of the Greenland Ice Sheet as a whole significantly, but not catastrophically, in the 21st century and beyond.

Greve, Ralf

2009-01-01T23:59:59.000Z

35

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]

Effect of the potential melting of the Greenland Ice Sheet on the Meridional Overturning February 2011 Keywords: Atlantic Meridional Overturning Circulation Sea level Greenland Ice Sheet Global of the Greenland Ice Sheet since the mid-1990s. This increased ice sheet mass loss might be an evidence of global

Han, Weiqing

36

Did changes in the Subpolar North Atlantic trigger the recent mass loss from the Greenland Ice Sheet?  

E-Print Network [OSTI]

Did changes in the Subpolar North Atlantic trigger the recent mass loss from the Greenland Ice) Leigh A. Stearns (University of Kansas) The Greenland Ice Sheet's (GIS) contribution to sea level rise and nearly-simultaneous acceleration of several outlet glaciers in Greenland's western and southeastern

Straneo, Fiamma

37

Modelling the hydrology of the Greenland ice sheet  

E-Print Network [OSTI]

This thesis aims to better understand the relationships between basal water pressure, friction, and sliding mechanisms at ice sheet scales. In particular, it develops a new subglacial hydrology model (Hydro) to explicitly ...

Karatay, Mehmet Rahmi

2011-06-28T23:59:59.000Z

38

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

E-Print Network [OSTI]

High-Resolution Monitoring of Internal Layers Over the Greenland Ice Sheet P. Kanagaratnam, S ice plays an important role in the rise of the Earth's sea level. A key variable in assessing the mass balance of an ice sheet is accumulation rate, which is currently determined from ice cores and pits

Kansas, University of

39

Evolution of supra-glacial lakes across the Greenland Ice Sheet  

E-Print Network [OSTI]

We used 268 cloud-free Moderate-resolution Imaging Spectroradiometer (MODIS) images spanning the melt seasons 2003 and 2005-2007 to study the seasonal evolution of supra-glacial lakes in three different regions of the Greenland ice sheet. Lake area...

Sundal, Aud

2008-12-05T23:59:59.000Z

40

Focused synthetic aperture radar processing of ice-sounder data collected over the Greenland ice sheet  

E-Print Network [OSTI]

We developed a synthetic aperture radar (SAR) processing algorithm for airborne/spaceborne ice-sounding radar systems and applied it to data collected in Greenland. By using focused SAR (phase-corrected coherent averaging), we improved along...

Legarsky, J.; Gogineni, Sivaprasad; Akins, T. L.

2001-10-01T23:59:59.000Z

Note: This page contains sample records for the topic "greenland ice sheet" 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

Using ice cores from the East Antarctic Ice Sheet, scientists have been able to study  

E-Print Network [OSTI]

Using ice cores from the East Antarctic Ice Sheet, scientists have been able to study ice's ice sheets. Ice sheets are huge areas of permanent ice. There are only three ice sheets on Earth: the Greenland Ice Sheet, the West Antarctic Ice Sheet, and the East Antarctic Ice Sheet. The Greenland Ice Sheet

42

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

43

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.

44

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

E-Print Network [OSTI]

oscillations and seasonal ice mass fluctuations, Eos Trans.2007), Rapid changes in ice discharge from Greenland outletW. et al. (2004), Greenland Ice Sheet: Increased coastal

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

2010-01-01T23:59:59.000Z

45

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

46

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

SciTech Connect (OSTI)

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

47

Determining Greenland Ice Sheet sensitivity to regional climate change: one-way coupling of a 3-D thermo-mechanical ice sheet model with a mesoscale climate model  

E-Print Network [OSTI]

Jakobshavn I. Rinks Observed Historic Flux (km 3 ice/year)I. Rinks * Outlets fed by the Northeast Greenland Ice StreamRinks, measured in 2000). Figure 3.1: Steady-state (A) topography (m) and (C) ice

Schlegel, Nicole-Jeanne

2011-01-01T23:59:59.000Z

48

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

SciTech Connect (OSTI)

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

49

Elastic uplift in southeast Greenland due to rapid ice mass loss Shfaqat A. Khan,1  

E-Print Network [OSTI]

Elastic uplift in southeast Greenland due to rapid ice mass loss Shfaqat A. Khan,1 John Wahr,2] The rapid unloading of ice from the southeastern sector of the Greenland ice sheet between 2001 and 2006), Elastic uplift in southeast Greenland due to rapid ice mass loss, Geophys. Res. Lett., 34, L21701, doi:10

Larson, Kristine

50

Climate-driven interannual ice mass evolution in Greenland I. Bergmanna  

E-Print Network [OSTI]

Climate-driven interannual ice mass evolution in Greenland I. Bergmanna , G. Ramillienb , FUniversite de Toulouse, UPS, OMP, GET, Toulouse, France Abstract We re-evaluate the Greenland mass balance of the Greenland Ice Sheet (GrIS), especially the recent deceleration of ice loss in 2009-2010, once seasonal

Paris-Sud XI, Universit de

51

NOTES AND CORRESPONDENCE Surface Melting over Ice Shelves and Ice Sheets as Assessed from Modeled  

E-Print Network [OSTI]

NOTES AND CORRESPONDENCE Surface Melting over Ice Shelves and Ice Sheets as Assessed from Modeled of ice shelves and their progenitor ice sheets. To explore the magnitude of surface melt occurring over) and most of the Greenland Ice Sheet (GIS) by the year 2500. Capping CO2 concentrations at present

Meissner, Katrin Juliane

52

MODIS snow albedo bias at high solar zenith angles relative to theory and to in situ observations in Greenland  

E-Print Network [OSTI]

glacial lakes across the Greenland Ice Sheet. Remote Sensing2000. Online article: Greenland climate network (GC- Net)characteristics on the Greenland Ice Sheet using MODIS and

Wang, Xianwei; Zender, Charles S

2010-01-01T23:59:59.000Z

53

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.

54

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

E-Print Network [OSTI]

temperatures directly from the Greenland Ice Sheet. Science2006. The 8.2ka event from Greenland ice cores. QuaternaryJouzel, Isotope calibrated Greenland temperature record over

Kobashi, Takuro

2007-01-01T23:59:59.000Z

55

Postdoctoral position Antarctic ice sheet modelling Free University of Brussels (VUB)  

E-Print Network [OSTI]

systems and ice caps, and in ice sheets in both polar regions (Greenland and Antarctica). The project as improved treatments for basal processes (basal sliding below ice sheet, basal melting below ice shelvesPostdoctoral position Antarctic ice sheet modelling Free University of Brussels (VUB) The Ice

Huybrechts, Philippe

56

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

SciTech Connect (OSTI)

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

57

A new bed elevation dataset for Greenland  

E-Print Network [OSTI]

and bed data set for the Greenland ice sheet 1. Measure-bed elevation dataset for Greenland J. L. Bamber 1 , J. A.face mass balance of the Greenland ice sheet revealed by

2013-01-01T23:59:59.000Z

58

Satellite investigations of ice dynamics and supraglacial lake development in Greenland  

E-Print Network [OSTI]

This thesis aims to improve the current understanding of the processes which control the flow variability of Greenland Ice Sheet (GrIS) outlet glaciers. The most recent Intergovernmental Governmental Panel on Climate ...

Briggs, Kate Hannah

2012-06-25T23:59:59.000Z

59

Received 26 Aug 2013 | Accepted 22 Apr 2014 | Published 21 May 2014 Ice sheets as a significant source of highly  

E-Print Network [OSTI]

, but are rarely considered as active components of the global iron cycle. The ocean waters around both ice sheets, Katherine Lee1 & Jon Telling1 The Greenland and Antarctic Ice Sheets cover B10% of global land surface concentrations in subglacial runoff from a large Greenland Ice Sheet catchment reveal the potential for globally

Benning, Liane G.

60

Elastic uplift in southeast Greenland due to rapid ice mass loss  

E-Print Network [OSTI]

[1] The rapid unloading of ice from the southeastern sector of the Greenland ice sheet between 2001 and 2006 caused an elastic uplift of ?35 mm at a GPS site in Kulusuk. Most of the uplift results from ice dynamic-induced volume losses on two nearby...

Khan, Shfaqat A.; Wahr, John; Stearns, Leigh; Hamilton, Gordon; van Dam, Tonie; Larson, Kristine M.; Francis, Olivier

2007-11-01T23:59:59.000Z

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


61

Global ice sheet modeling  

SciTech Connect (OSTI)

The University of Maine conducted this study for Pacific Northwest Laboratory (PNL) as part of a global climate modeling task for site characterization of the potential nuclear waste respository site at Yucca Mountain, NV. The purpose of the study was to develop a global ice sheet dynamics model that will forecast the three-dimensional configuration of global ice sheets for specific climate change scenarios. The objective of the third (final) year of the work was to produce ice sheet data for glaciation scenarios covering the next 100,000 years. This was accomplished using both the map-plane and flowband solutions of our time-dependent, finite-element gridpoint model. The theory and equations used to develop the ice sheet models are presented. Three future scenarios were simulated by the model and results are discussed.

Hughes, T.J.; Fastook, J.L. [Univ. of Maine, Orono, ME (United States). Institute for Quaternary Studies

1994-05-01T23:59:59.000Z

62

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

63

The Melting of Greenland William H. Lipscomb  

E-Print Network [OSTI]

). AnAn ice capice cap is a mass of glacier ice smaller than 50,000 kmis a mass of glacier ice smaller is negligibleSurface melting is negligible Antarctic ice thicknessAntarctic ice thickness (British Antarctic of the Greenland iceMuch of the Greenland ice sheet may have meltedsheet may have melted Greenland minimum extent

Born, Andreas

64

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

SciTech Connect (OSTI)

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

65

Constraining MODIS snow albedo at large solar zenith angles: Implications for the surface energy budget in Greenland  

E-Print Network [OSTI]

surface albedo of the Greenland ice sheet: satellite-derivedand J. Box. 2001. Surface climatology of the Greenland IceSheet: Greenland climate net- work 1995-1999. J. Geophys.

Wang, Xianwei; Zender, Charles S

2010-01-01T23:59:59.000Z

66

Holocene sea-ice variations in Greenland: onshore evidence  

E-Print Network [OSTI]

Holocene sea-ice variations in Greenland: onshore evidence Ole Bennike* (Geological Survey of Denmark and Greenland, ster Voldgade 10, DK-1350 Copenhagen K, Denmark) Received 12 August 2002; revised manuscript accepted 2 April 2003 Abstract: The oldest dated driftwood log from northern Greenland is c. 9300

Inglfsson, lafur

67

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

E-Print Network [OSTI]

firn and ice at Summit, Greenland, J. Geophys. Res. , 98,AL. : TRACE GASES IN GREENLAND ICE CORE . Andreae Kettle,and sulfur gases from Greenland ice cores M. Aydin, 1 M. B.

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

2007-01-01T23:59:59.000Z

68

Home Atmosphere Sea Ice Ocean Land Greenland Biology , L.-S. Bai  

E-Print Network [OSTI]

Home Atmosphere Sea Ice Ocean Land Greenland Biology Greenland J. E. Box 1 , L.-S. Bai 1 , R across the southern half of Greenland led to substantially higher west coast sea ice thickness and concentration. Even so, record-setting summer temperatures around Greenland, combined with an intense melt

Box, Jason E.

69

2, 879921, 2006 Ice-sheet evolution  

E-Print Network [OSTI]

CPD 2, 879921, 2006 Ice-sheet evolution during the last climatic cycle S. Charbit et al. Title reconstructions of the Northern Hemisphere ice sheets through the last glacial-interglacial cycle S. Charbit1 , C921, 2006 Ice-sheet evolution during the last climatic cycle S. Charbit et al. Title Page Abstract

Boyer, Edmond

70

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

71

A tentative reconstruction of the last interglacial and glacial inception in Greenland based on new gas measurements in the Greenland Ice  

E-Print Network [OSTI]

A tentative reconstruction of the last interglacial and glacial inception in Greenland based on new gas measurements in the Greenland Ice Core Project (GRIP) ice core Amaelle Landais,1 Je September 2003. [1] The disturbed stratigraphy of the ice in the lowest 10% of the Greenland GRIP ice core

Chappellaz, Jrme

72

Greenland snow accumulation estimates from satellite radar scatterometer data  

E-Print Network [OSTI]

Greenland snow accumulation estimates from satellite radar scatterometer data Mark R. Drinkwater accumulation on the Greenland ice sheet. Microwave radar backscatter images of Greenland are derived using (or decrease) in net snow accumulation on the polar ice caps. The net mass balance of the Greenland

Long, David G.

73

Interannual variability of Arctic sea ice export into the East Greenland Current  

E-Print Network [OSTI]

Interannual variability of Arctic sea ice export into the East Greenland Current K. A. Cox,1 J. D cycle, Arctic sea ice decline, and increasing Greenland glacial melt. Here we use new d18 O data from the East Greenland Current system at Cape Farewell and Denmark Strait to determine the relative proportions

Rohling, Eelco

74

A 600-year annual 10 Be record from the NGRIP ice core, Greenland  

E-Print Network [OSTI]

A 600-year annual 10 Be record from the NGRIP ice core, Greenland A.-M. Berggren,1 J. Beer,2 G only one record (Dye-3, Greenland) providing annual resolution over several centuries. Here we report the NGRIP site in Greenland. NGRIP and Dye-3 10 Be exhibits similar long-term variability, although

Wehrli, Bernhard

75

GREENLAND INLAND ICE MELT-OFF: ANALYSIS OF GLOBAL GRAVITY DATA FROM THE GRACE SATELLITES  

E-Print Network [OSTI]

GREENLAND INLAND ICE MELT-OFF: ANALYSIS OF GLOBAL GRAVITY DATA FROM THE GRACE SATELLITES Allan A) in meters starting at 29 July 2002 and ending at 25 August 2010. Results focussing on Greenland show indications of a transition taking place in the mass loss in Greenland from mid-2004 to early 2006. Index

76

Ice-front variation and tidewater behavior on Helheim and Kangerdlugssuaq Glaciers, Greenland  

E-Print Network [OSTI]

Ice-front variation and tidewater behavior on Helheim and Kangerdlugssuaq Glaciers, Greenland Ian Glaciers, Greenland, from 2001 to 2006, a period in which they retreated and sped up. These data show and retreat in less than a century indicates that tidewater glaciers in Greenland can advance rapidly

Tsai, Victor C.

77

A New Coherent Radar for Ice Sounding in Greenland A. Moussessian  

E-Print Network [OSTI]

A New Coherent Radar for Ice Sounding in Greenland A. Moussessian 1 , R.L. Jordan 1 , E. Rodriguez of this radar on board a P-3 aircraft took place in May of 1999 over Greenland with successful results blanking. The first deployment of this radar took place in May of 1999 in Greenland. During this deployment

Kansas, University of

78

EnvironmentThe MIT Press 2011 The Fate of Greenland  

E-Print Network [OSTI]

EnvironmentThe MIT Press 2011 #12;NEW The Fate of Greenland Lessons from Abrupt Climate Change above, Greenland offers an endless vista of whiteness interrupted only by scattered ponds of azure-colored melt water. Ninety percent of Greenland is covered by ice; its ice sheet, the largest outside

Jackson, Daniel

79

Advanced Review Greenland climate change: from  

E-Print Network [OSTI]

Advanced Review Greenland climate change: from the past to the future Valerie Masson-Delmotte,1 cores in and around Greenland allow us to place the current trends in regional climate, ice sheet lake sediments in southern Greenland document major environmental and climatic conditions during

Bhatt, Uma

80

IDENTIFYING ICE HYDROMETEOR SIGNATURES ABOVE SUMMIT, GREENLAND USING A MULTI-INSTRUMENT APPROACH  

E-Print Network [OSTI]

IDENTIFYING ICE HYDROMETEOR SIGNATURES ABOVE SUMMIT, GREENLAND USING A MULTI. These retrievals, however, may be adversely affected by ice hydrometeors commonly observed in mixed phase clouds. Research on the effect of ice hydrometeors on the microwave signal is insufficient. We establish that ice

Wisconsin at Madison, University of

Note: This page contains sample records for the topic "greenland ice sheet" 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

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

E-Print Network [OSTI]

, and sulfur gases from Greenland ice cores M. Aydin,1 M. B. Williams,1 and E. S. Saltzman1 Received 7-lived atmospheric trace gases were measured in 25 ice core samples from Summit, Greenland. Samples were selected. The CH3Br results are consistent with previous observations of ``excess'' CH3Br in Greenland firn air

Saltzman, Eric

82

Neglecting ice-atmosphere interactions underestimates ice sheet melt in millennial-scale deglaciation simulations  

E-Print Network [OSTI]

Laurentide and Innutian ice sheets during the Last Glacialclimate of the laurentide ice sheet at the LGM, J. Clim. ,1958), The flow law of ice: A discussion of the assumptions

Pritchard, M. S.; Bush, A. B.; Marshall, S. J.

2008-01-01T23:59:59.000Z

83

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

E-Print Network [OSTI]

that a reduction in sea ice extent in the North Atlantic produces a climatic response consistent with abruptAbrupt climate shifts in Greenland due to displacements of the sea ice edge Camille Li,1 David S ice could be changes in ocean thermohaline circulation (OTC) or rearrangements of the tropical

Schrag, Daniel

84

greenland Field seminar The integrating experience of the IGErT traineeship is  

E-Print Network [OSTI]

greenland Field seminar The integrating experience of the IGErT traineeship is the Greenland Field processes on the Greenland ice sheet at Summit Camp, and environmental policy and science communication in Nuuk, the capital of Greenland. The Dartmouth IGErT is administered by the Institute of arctic Studies

Lotko, William

85

SeaWinds views Greenland Ivan S. Ashcraft and David G. Long  

E-Print Network [OSTI]

SeaWinds views Greenland Ivan S. Ashcraft and David G. Long Brigham Young University, MERS facies in Greenland. The duration of the summer melt over the Greenland ice sheet is calculated using backscatter images of Greenland are produced to investigate diurnal varia- tions in backscatter measurements

Long, David G.

86

Bacteria beneath the West Antarctic Ice Sheet Brian Lanoil,1  

E-Print Network [OSTI]

Bacteria beneath the West Antarctic Ice Sheet Brian Lanoil,1 * Mark Skidmore,1 John C. Priscu,2, particularly those that lie beneath polar ice sheets, are beginning to be recog- nized as an important part Vostok, Antarctica, no sub-ice sheet environments have been shown to support microbial ecosystems. Here

Priscu, John C.

87

Microstructure through an ice sheet Tobias Binder1, a  

E-Print Network [OSTI]

Microstructure through an ice sheet Tobias Binder1, a , Ilka Weikusat2, b , Johannes Freitag2, c.Garbe@iwr.uni-heidelberg.de, e Dietmar.Wagenbach@iup.uni-heidelberg.de, f Sepp.Kipfstuhl@awi.de Keywords: Ice, microstructure characterization, grain boundary curvature, image processing Abstract. Ice cores through an ice sheet can

Garbe, Christoph S.

88

Greenland Observed at High Resolution by the Seasat Scatterometer  

E-Print Network [OSTI]

Greenland Observed at High Resolution by the Seasat Scatterometer D.G. Long', P.J. Hardin2, and RA to SASS data for the study of Greenland's ice sheet. We present a time series of the radar backscatter images over Greenland covering the time period July-September 1978. The images provide an island

Long, David G.

89

West antarctic ice sheet collapse: Chimera or clear danger  

SciTech Connect (OSTI)

The specter of a west antarctic collapse has been with us for 25 years. Recently, certain official assessments concerned primarily with the future response to projected global warming have concluded that Antarctica will not cause much sea-level rise within the planning horizon of a century or so. At the same time startling new results on ice sheet (in)stability have been emerging, pointing to less stability then previously believed. Some recent results are reviewed briefly: Heinrich layers in the North Atlantic show basally lubricated surges of the Laurentide ice sheet; the west antarctic ice sheet collapsed recently; the modern west antarctic ice sheet is changing rapidly locally; the bed of ice stream B is exceptionally well lubricated by water and water-saturated soft sediments; the modern ice sheet is thinning slowly on average; a model west antarctic ice sheet undergoes rapid collapses long after forcing and probably related to penetration of warmth to the bed. 23 refs.

Alley, R.B. (Pennsylvania State Univ., University Park, PA (United States)); MacAyeal, D.R. (Univ. of Chicago, IL (United States))

1993-01-01T23:59:59.000Z

90

ICE SHEET SOURCES OF SEA LEVEL RISE AND FRESHWATER DISCHARGE  

E-Print Network [OSTI]

ICE SHEET SOURCES OF SEA LEVEL RISE AND FRESHWATER DISCHARGE DURING THE LAST DEGLACIATION Anders E the sources of sea level rise and freshwater dis- charge to the global oceans associated with retreat of ice­10 m sea level rise at 19.0­19.5 ka, sourced largely from Northern Hemisphere ice sheet retreat

Carlson, Anders

91

The Need for SPIRIT DEMs to Quantify Antarctic Ice Sheet  

E-Print Network [OSTI]

appropriate mask ­ SPIRIT has the data and could produce the necessary DEMs #12;Conclusions · Antarctic iceThe Need for SPIRIT DEMs to Quantify Antarctic Ice Sheet Discharge Robert Bindschadler NASA & UMBC #12;Antarctic Ice Sheet Discharge · 33 largest, most active basins account for 840 Gt/a (Rignot

Berthier, Etienne

92

Numerical Age Computation of the Antarctic Ice Sheet for Dating Deep Ice Cores  

E-Print Network [OSTI]

Numerical Age Computation of the Antarctic Ice Sheet for Dating Deep Ice Cores Bernd M¨ugge1 for the computation of the age of ice is discussed within the frame of numerical ice sheet modelling. The first method of a numerical diffusion term to stabilize the solution and therefore produces arbitrary results in a near

Calov, Reinhard

93

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.

94

Ice Thickness Measurements of the Southwest Greenland 2000-m Contour Line J. J. Legarsky, S.P. Gogineni, P. Kanagaratnam, T. L. Akins and Y. C. Wong  

E-Print Network [OSTI]

Ice Thickness Measurements of the Southwest Greenland 2000-m Contour Line J. J. Legarsky, S Laborato~ performed ice thickness measurements along several flights in the southern part of Greenland. We of the Greenland. INTRODUCTION Since 1993, we have been performing radar ice thickness measurements as a part

Kansas, University of

95

Sandia National Laboratories: Ice-Sheet Simulation Code Matures...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

and Antarctic Ice Sheets, with particular attention to their contributions to global sea-level rise. Our recent highlight is the successful completion of a controlled mesh...

96

Modeling the evolution of polar ice sheets: Ice sheet system model workshop; Bergen, Norway, 2-4 June 2014  

E-Print Network [OSTI]

Model Workshop; Bergen, Norway, 2?4 June 2014 The Ice SheetUniversity of Bergen in Norway, in June 2014. This is the

Larour, E; Schlegel, N; Morlighem, M

2014-01-01T23:59:59.000Z

97

Past Accumulation Rates of the Western Antarctic Ice Sheet Near an Ice Divide  

E-Print Network [OSTI]

The study of accumulation rates of ice is a direct link to the evolution of ice sheet. It is believed by scientists that ice sheet evolution will aid in the mystery of climate change and may lead to predictions about climates in the future...

Child, Sarah

2009-08-12T23:59:59.000Z

98

The last Scandinavian Ice Sheet in northwestern Russia: ice flow patterns and decay dynamics  

E-Print Network [OSTI]

U N C O R R EC TED PR O O F The last Scandinavian Ice Sheet in northwestern Russia: ice flow Sheet in northwestern Russia: ice flow patterns and decay dynamics. Boreas, Vol. 35, pp. xxxÁxxx. Oslo) in northwestern Russia took place after a period of periglacial conditions. Till of the last SIS, Bobrovo till

Ingólfsson, ?lafur

99

Levoglucosan as a specific marker of fire events in Greenland snow  

E-Print Network [OSTI]

Levoglucosan as a specific marker of fire events in Greenland snow By NATALIE KEHRWALD1 *, ROBERTA collected from a 3 m snow pit at Summit, Greenland (72820?N, 38845?W; 3270 m a.s.l.), with a known, through their eastward transport and deposition on the Greenland ice sheet, and their eventual burial

Paris-Sud XI, Universit de

100

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

E-Print Network [OSTI]

Response of a marineterminating Greenland outlet glacier to abrupt cooling 8200 and 9300 years ago 16 December 2011. [1] Longterm records of Greenland outletglacier change extending beyond the satellite era can inform future predictions of Greenland Ice Sheet behavior. Of particular relevance

Briner, Jason P.

Note: This page contains sample records for the topic "greenland ice sheet" 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

The deglaciation and neoglaciation of Upernavik Isstrm, Greenland Jason P. Briner a,  

E-Print Network [OSTI]

The deglaciation and neoglaciation of Upernavik Isstrm, Greenland Jason P. Briner a, , Lena Geological Survey of Denmark and Greenland, ster Voldgade 10, 1350 Copenhagen-K, Denmark c Department 2013 Available online 21 October 2013 Keywords: Greenland Ice Sheet Upernavik Isstrm Holocene

Briner, Jason P.

102

High variability of Greenland surface temperature over the past 4000 years estimated from trapped air  

E-Print Network [OSTI]

High variability of Greenland surface temperature over the past 4000 years estimated from trapped 10 October 2011; accepted 11 October 2011; published 10 November 2011. [1] Greenland recently is impacting the Greenland ice sheet and in turn accelerating global sealevel rise. Yet, it remains imprecisely

Severinghaus, Jeffrey P.

103

Increasing Temporal Resolution in Greenland Ablation Estimation Using Passive and Active Microwave Data  

E-Print Network [OSTI]

Increasing Temporal Resolution in Greenland Ablation Estimation Using Passive and Active Microwave of these measurements provides an increased understanding of the diurnal melt cycle over Greenland and estimation of the melt profile. I. INTRODUCTION Accurate estimation of the mass balance of the Greenland ice sheet

Long, David G.

104

Ice Stream C slowdown is not stabilizing West Antarctic Ice Sheet S Anandakrishnan RB Alleyy  

E-Print Network [OSTI]

Ice Stream C slowdown is not stabilizing West Antarctic Ice Sheet S Anandakrishnan RB Alleyy RW Jacobelz H Conwayx March 24, 1999 Abstract Changes in the flow of ice stream C likely indicate a continuing part of ice stream C, West Antarctica largely stagnated over the last few centuries, while upglacier

Jacobel, Robert W.

105

Modeling the Fracture of Ice Sheets on Parallel Computers  

SciTech Connect (OSTI)

The objective of this project was to investigate the complex fracture of ice and understand its role within larger ice sheet simulations and global climate change. This objective was achieved by developing novel physics based models for ice, novel numerical tools to enable the modeling of the physics and by collaboration with the ice community experts. At the present time, ice fracture is not explicitly considered within ice sheet models due in part to large computational costs associated with the accurate modeling of this complex phenomena. However, fracture not only plays an extremely important role in regional behavior but also influences ice dynamics over much larger zones in ways that are currently not well understood. To this end, our research findings through this project offers significant advancement to the field and closes a large gap of knowledge in understanding and modeling the fracture of ice sheets in the polar regions. Thus, we believe that our objective has been achieved and our research accomplishments are significant. This is corroborated through a set of published papers, posters and presentations at technical conferences in the field. In particular significant progress has been made in the mechanics of ice, fracture of ice sheets and ice shelves in polar regions and sophisticated numerical methods that enable the solution of the physics in an efficient way.

Waisman, Haim [Columbia University] [Columbia University; Tuminaro, Ray [Sandia National Labs] [Sandia National Labs

2013-10-10T23:59:59.000Z

106

Laurentide Ice Sheet meltwater and abrupt climate change during the last glaciation  

SciTech Connect (OSTI)

A leading hypothesis to explain abrupt climate change during the last glacial cycle calls on fluctuations in the margin of the North American Laurentide Ice Sheet (LIS), which may have routed freshwater between the Gulf of Mexico (GOM) and North Atlantic, affecting North Atlantic Deep Water (NADW) variability and regional climate. Paired measurements of {delta}O and Mg/Ca of foraminiferal calcite from GOM sediments reveal five episodes of LIS meltwater input from 28-45 thousand years ago (ka) that do not match the millennial-scale Dansgaard-Oeschger (D/O) warmings recorded in Greenland ice. We suggest that summer melting of the LIS may occur during Antarctic warming and likely contributed to sea-level variability during Marine Isotope Stage 3 (MIS 3).

Hill, H W; Flower, B P; Quinn, T M; Hollander, D J; Guilderson, T P

2005-10-02T23:59:59.000Z

107

Changes in Sea-Level associated with Modi cations of the Mass Balance of the Greenland and Antarctic  

E-Print Network [OSTI]

Changes in Sea-Level associated with Modi cations of the Mass Balance of the Greenland and Antarctic Ice Sheets over the 21st Century V eronique Bugnion Abstract Changes in runo from Greenland for estimating melting and runo . All models are solved on 20 and 40 km grids respectively for Greenland

108

Numerical modelling of ice sheets, streams, and shelves  

E-Print Network [OSTI]

Numerical modelling of ice sheets, streams, and shelves Ed Bueler Karthaus, September 2012 models can actually help you, the reader, understand the behavior of partic- ular ice flows. Their most numerical codes produce numbers, but we want numbers that actually come from our continuum model. We analyse

Bueler, Ed

109

An in situ measurement of the radio-frequency attenuation in ice at Summit Station, Greenland  

E-Print Network [OSTI]

We report an in situ measurement of the electric field attenuation length at radio frequencies for the bulk ice at Summit Station, Greenland, made by broadcasting radio-frequency signals vertically through the ice and measuring the relative power in the return ground bounce signal. We find the depth-averaged field attenuation length to be 947 +92/-85 meters at 75 MHz. While this measurement has clear radioglaciological applications, the radio clarity of the ice also has implications for the detection of ultra-high energy (UHE) astrophysical particles via their radio emission in dielectric media such as ice. The measured attenuation length at Summit Station is comparable to previously measured radio-frequency attenuation lengths at candidate particle detector sites around the world, and strengthens the case for Summit Station as the most promising northern site for UHE neutrino detection.

J. Avva; J. M. Kovac; C. Miki; D. Saltzberg; A. G. Vieregg

2014-09-30T23:59:59.000Z

110

Grounding-line migration in plan-view marine ice-sheet models: results of the ice2sea MISMIP3d intercomparison  

E-Print Network [OSTI]

models (SSA, AHySSA) produce larger ice sheets than modelsplan-view ice-sheet models they produce different results.the Antarctic ice sheet should at least produce grounding-

2013-01-01T23:59:59.000Z

111

Ice sheets and their dynamics Continuum thermo-mechanical model of a glacier  

E-Print Network [OSTI]

Ice sheets and their dynamics Continuum thermo-mechanical model of a glacier Shallow Ice Approximation (SIA) SIA-I Iterative Improvement Technique Benchmarks Numerical modeling of ice-sheet dynamics and Cartography, Zdiby 1.6.2010 Ondej Soucek Ph.D. defense #12;Ice sheets and their dynamics Continuum thermo

Cerveny, Vlastislav

112

Adaptive mesh, finite volume modeling of marine ice sheets Stephen L. Cornforda  

E-Print Network [OSTI]

Adaptive mesh, finite volume modeling of marine ice sheets Stephen L. Cornforda , Daniel F. Martinb Abstract Continental scale marine ice sheets such as the present day West Antarctic Ice Sheet are strongly phenomenon of this kind is the migration of the grounding line -- the division between ice in contact

113

Complex systems influence melting of Greenland ice sheet  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr MayAtmospheric Optical Depth7-1D: Vegetation Proposed New SubstationCleanCommunity Involvement andMISR, and4 NComplex

114

Team advances understanding of the Greenland Ice Sheet's meltwater  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May JunDatastreamsmmcrcalgovInstrumentsrucLas ConchasPassiveSubmittedStatus TomAboutManus Site-InactiveLaboratoryTeam

115

Hydrology and dynamics of a land-terminating Greenland outlet glacier  

E-Print Network [OSTI]

The purpose of this thesis is to investigate the hydrology and dynamics of a land-terminating outlet glacier on the western margin of the Greenland Ice Sheet (GrIS). The investigations are motivated by uncertainty about ...

Bartholomew, Ian David

2012-11-29T23:59:59.000Z

116

Supraglacial lakes on the Larsen B Ice Shelf, Antarctica, and Paakitsoq Region, Greenland: a comparative study  

E-Print Network [OSTI]

.epsl.2011.04.014. 427 Box, J. E., and K. Ski (2007), Remote sounding of Greenland supraglacial melt lakes: 428 implications for subglacial hydraulics, J. Glaciol., 53(181), 257265, 429 doi:10.3189/172756507782202883. 430 Bromwich, D. H., J. P. Nicolas... , Geophys. Res. Lett., 39(16), L16504, 510 doi:10.1029/2012GL052413. 511 Mobley, C. D. (1994), Light and water: radiative transfer in natural waters. 512 Academic Press, San Diego, 592. 513 Phillips, H. A. (1998), Surface meltstreams on the Amery Ice...

Banwell, Alison F.; Caballero, Martamaria; Arnold, Neil S.; Glasser, Neil F.; Cathles, L. Mac; MacAyeal, Douglas R.

2014-05-01T23:59:59.000Z

117

Interannual Atmospheric Variability Affects Continental Ice Sheet Simulations on Millennial Time Scales  

E-Print Network [OSTI]

well as cooling at the southeast margin of the ice sheet. Fdue to cooling over the North Ameri- can and Eurasian icetide ice sheet margin resulting in a 1C cooling over the

Pritchard, Michael S; Bush, Andrew B. G; Marshall, Shawn J

2008-01-01T23:59:59.000Z

118

ICE SHEETS, GLOBAL WARMING, AND ARTICLE 2 OF THE UNFCCC An Editorial Essay  

E-Print Network [OSTI]

such rapid-loss mechanisms, models cannot produce a stable ice sheet above some local warming thresholdICE SHEETS, GLOBAL WARMING, AND ARTICLE 2 OF THE UNFCCC An Editorial Essay 1. Introduction Rapid disintegration of the West Antarctic ice sheet (WAIS) was cited decades ago as a potentially severe consequence

Oppenheimer, Michael

119

Sensitivity of Cenozoic Antarctic ice sheet variations to geothermal heat flux  

E-Print Network [OSTI]

Sensitivity of Cenozoic Antarctic ice sheet variations to geothermal heat flux David Pollard a sheet to geothermal heat flux is investigated, using a coupled climate­ice sheet model with various prescribed values and patterns of geothermal heat flux. The sudden growth of major ice across the Eocene

120

TERAGRID 2007 CONFERENCE, MADISON, WI 1 Cyberinfrastructure for Remote Sensing of Ice Sheets  

E-Print Network [OSTI]

TERAGRID 2007 CONFERENCE, MADISON, WI 1 Cyberinfrastructure for Remote Sensing of Ice Sheets Dr rise and melting ice sheets is the application domain of this project. It is an issue of global impor of computationally intensive tools and models that will help them measure and predict the response of ice sheets

Note: This page contains sample records for the topic "greenland ice sheet" 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

Increasing the Scalability of PISM for High Resolution Ice Sheet Models Phillip Dickens  

E-Print Network [OSTI]

Increasing the Scalability of PISM for High Resolution Ice Sheet Models Phillip Dickens School at large. One important piece of the climate puzzle is how the dynamics of large-scale ice sheets developed several simulation models to predict and understand the behavior of large-scale ice sheets

Dickens, Phillip M.

122

Intelligent Matchmaking for Polar Ice Sheet Data Collection and Delivery  

E-Print Network [OSTI]

of intelligent radars integrated into robotic vehicles. They autonomously decide where and how to measure to map near- surface layers. These sensors are integrated into two vehicles; an autonomous robotic Abstract-- The PRISM (Polar Radar for Ice Sheet Measurement) project is developing mobile, autonomous

Kansas, University of

123

ESTIMATING BEDROCK AND SURFACE LAYER BOUNDARIES AND CONFIDENCE INTERVALS IN ICE SHEET RADAR IMAGERY USING MCMC  

E-Print Network [OSTI]

ESTIMATING BEDROCK AND SURFACE LAYER BOUNDARIES AND CONFIDENCE INTERVALS IN ICE SHEET RADAR IMAGERY and Computing Indiana University Bloomington, Indiana USA ABSTRACT Climate models that predict polar ice sheet behavior require accurate measurements of the bedrock-ice and ice-air bound- aries in ground

Menczer, Filippo

124

Time-variable gravity observations of ice sheet mass balance: Precision and limitations of the GRACE satellite data  

E-Print Network [OSTI]

observations, Science, 314, Peltier, W. R. (2004), Globalice history models (ICE5G [Peltier, 2004] and Fleming andfor Greenland; ICE5G [Peltier, 2004] and IJ05 [Ivins and

Velicogna, I.; Wahr, J.

2013-01-01T23:59:59.000Z

125

FactSheet-TWP_ICE.indd  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr MayAtmospheric Optical Depth7-1D: Vegetation ProposedUsing ZirconiaPolicy andExsolutionFES6FYRANDOM DRUG TESTINGJanuaryFact SheetsARMWarm

126

Hysteresis in Cenozoic Antarctic ice-sheet variations David Pollarda,*, Robert M. DeContob,1  

E-Print Network [OSTI]

., 2000). These and other data suggest a long period of virtually ice-free cooling during the EoceneHysteresis in Cenozoic Antarctic ice-sheet variations David Pollarda,*, Robert M. DeContob,1 A coupled global climate­Antarctic ice sheet model is run for 10 million years across the Eocene

127

A Computational Study of the Spreading of Oil Underneath a Sheet of Ice  

E-Print Network [OSTI]

A Computational Study of the Spreading of Oil Underneath a Sheet of Ice Mark Sussman Department) Abstract The spreading of oil underneath a sheet of ice is computed using an adaptive level set method the final steady profile of a body of oil under ice in water. The computational models are used to make

Soatto, Stefano

128

The sensitivity of the Late Saalian (140 ka) and LGM (21 ka) Eurasian ice sheets to sea surface conditions  

E-Print Network [OSTI]

to the climatic cooling effect from the large ice sheet topography. Late Saalian SST are simulated using an AGCM-hemispheric asymmetry caused by the larger ice-albedo feedback, cooling climate. The resulting Late Saalian ice sheetThe sensitivity of the Late Saalian (140 ka) and LGM (21 ka) Eurasian ice sheets to sea surface

Jakobsson, Martin

129

Geomorphology and dynamics of the British-Irish Ice Sheet in western Scotland  

E-Print Network [OSTI]

Predicting the long-term behaviour of present-day ice sheets is hampered by the short timescales of our observations and restricted knowledge of the subglacial environment. Studying palaeoice sheets can help by revealing ...

Finlayson, Andrew

2014-06-30T23:59:59.000Z

130

Where might we find evidence of a Last Interglacial West Antarctic Ice Sheet collapse in Antarctic ice core records?  

E-Print Network [OSTI]

increased melting from valley glaciers and small ice caps (estimated ~0.60.1 m, Radi and Hock, 2010), oceanWhere might we find evidence of a Last Interglacial West Antarctic Ice Sheet collapse in Antarctic ice core records? S.L. Bradley a, , M. Siddall a , G.A. Milne b , V. Masson-Delmotte c , E. Wolff d

Siddall, Mark

131

Simulation of the Fennoscandian ice sheet during the last glaciation using  

E-Print Network [OSTI]

sliding is triggered when basal temperatures reach melting point of ice sliding is proportional to power- mechanical ice sheet model coupled to an isostatic adjustment model. The model predicts thermal conditions

132

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.

133

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

134

Ice-sheet model sensitivities to environmental forcing and their use in projecting future sea level (the SeaRISE project)  

E-Print Network [OSTI]

for shallow polythermal ice sheets. Philos. Trans. R. Soc.doi:10.3189/2013JoG12J125 Ice-sheet model sensitivities to1993) On the initiation of ice sheets. Ann. Glaciol. , 18,

2013-01-01T23:59:59.000Z

135

Reconstruction of the Past and Forecast of the Future European and British Ice Sheets and Associated SeaLevel Change  

E-Print Network [OSTI]

The aim of this project is to improve our understanding of the past European and British ice sheets as a basis for forecasting their future. The behaviour of these ice sheets is investigated by simulating them using a ...

Hagdorn, Magnus K M

136

Marginal formations of the last Kara and Barents ice sheets in northern European Russia  

E-Print Network [OSTI]

Marginal formations of the last Kara and Barents ice sheets in northern European Russia VALERY I): Marginal formations of the last Kara and Barents ice sheets in northern European Russia. Boreas, Vol. 28, pp. 23­45. Oslo. ISSN 0300-9483. Glacial landforms in northern Russia, from the Timan Ridge

Ingólfsson, ?lafur

137

Ice sheet limits in Norway and on the Norwegian continental shelf Jan Mangerud  

E-Print Network [OSTI]

Ice sheet limits in Norway and on the Norwegian continental shelf Jan Mangerud University of Bergen, Department of Geology, Allégt. 41, N-5007 Bergen, Norway Jan.Mangerud@geol.uib.no Introduction Ice sheets the author will briefly review present knowledge of the glacial history of Norway. The recon- struction

Ingólfsson, ?lafur

138

The sedimentary record of subglacial erosion beneath the Laurentide Ice Sheet  

E-Print Network [OSTI]

The sedimentary record of subglacial erosion beneath the Laurentide Ice Sheet Gregory A. Balco Abstract The sedimentary record of subglacial erosion beneath the Laurentide Ice Sheet by Gregory A. Balco and Space Sciences I use measurements of the cosmic-ray-produced radionuclides 10 Be and 26 Al

Stone, John

139

View of NY harbor from the JOIDES Resolution in an ice-free world (73 m rise)  

E-Print Network [OSTI]

less dense global 20th century warming ~0.6C 1.6 mm/yr sea-level rise Melting Glaciers & Ice Caps? Melting Mountain Glaciers and Ice Caps: Alpine glaciers 0.6 mm/yr Greenland Ice Cap IPCC2001: near 0-80 cm IPPC 2007 error: 20-60 cm (does not include ice sheet melting) http

140

Effective stress profiles and seepage flows beneath glaciers and ice sheets  

E-Print Network [OSTI]

stress for ice infiltration Qb Heat flux into glacier base Qf Heat produced by dissipation Qg GeothermalEffective stress profiles and seepage flows beneath glaciers and ice sheets Alan W. REMPEL spacing and the heat-flow regime. Considerations of thermodynamic equilibrium require that ice penetrates

Rempel, Alan W.

Note: This page contains sample records for the topic "greenland ice sheet" 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

Orbital and CO2 forcing of late Paleozoic continental ice sheets Daniel E. Horton,1  

E-Print Network [OSTI]

) produce large changes in late Paleozoic ice volume ($1.3 ? 108 km3 ) and sea level ($20 to 245 m). Between cold summer orbit, but still produces significant ice volumes ($8­12 ? 107 km3 ). Our results highlightOrbital and CO2 forcing of late Paleozoic continental ice sheets Daniel E. Horton,1 Christopher J

Poulsen, Chris J.

142

Modelling West Antarctic ice sheet growth and collapse through the past five million years  

E-Print Network [OSTI]

, isolated ice caps on West Antarctic islands. Transitions between glacial, intermediate and collapsed states temperature and specified sea level. A new parameterization of sub- ice-shelf ocean melt based on modernLETTERS Modelling West Antarctic ice sheet growth and collapse through the past five million years

143

Eos, Vol. 91, No. 29, 20 July 2010 Water and wet sediments under ice sheets  

E-Print Network [OSTI]

Eos, Vol. 91, No. 29, 20 July 2010 Water and wet sediments under ice sheets can play an important role in regulating the rate of ice stream flow in Antarctica, particularly over short time scales. Indeed, the discharge of subglacial lakes has been linked to an increase in ice velocity of Byrd Glacier

Priscu, John C.

144

Ice-sheet model sensitivities to environmental forcing and their use in projecting future sea level (the SeaRISE project)  

E-Print Network [OSTI]

processes that can produce rapid ice loss, (2) large-scalesimulate the same ice sheet can produce different behaviorss. The Antarctic ice sheet is predicted to produce a greater

2013-01-01T23:59:59.000Z

145

Investigation of coastal dynamics of the Antarctic Ice Sheet using sequential Radarsat SAR images  

E-Print Network [OSTI]

Increasing human activities have brought about a global warming trend, and cause global sea level rise. Investigations of variations in coastal margins of Antarctica and in the glacial dynamics of the Antarctic Ice Sheet provide useful diagnostic...

Tang, Sheng-Jung

2009-05-15T23:59:59.000Z

146

A parallel high-order accurate finite element nonlinear Stokes ice sheet model and benchmark experiments  

SciTech Connect (OSTI)

The numerical modeling of glacier and ice sheet evolution is a subject of growing interest, in part because of the potential for models to inform estimates of global sea level change. This paper focuses on the development of a numerical model that determines the velocity and pressure fields within an ice sheet. Our numerical model features a high-fidelity mathematical model involving the nonlinear Stokes system and combinations of no-sliding and sliding basal boundary conditions, high-order accurate finite element discretizations based on variable resolution grids, and highly scalable parallel solution strategies, all of which contribute to a numerical model that can achieve accurate velocity and pressure approximations in a highly efficient manner. We demonstrate the accuracy and efficiency of our model by analytical solution tests, established ice sheet benchmark experiments, and comparisons with other well-established ice sheet models.

Leng, Wei [Chinese Academy of Sciences; Ju, Lili [University of South Carolina; Gunzburger, Max [Florida State University; Price, Stephen [Los Alamos National Laboratory; Ringler, Todd [Los Alamos National Laboratory,

2012-01-01T23:59:59.000Z

147

Scalable, Efficient, and Accurate Community Ice Sheet Model (SEACISM) PRINCIPAL INVESTIGATOR: Katherine J. Evans  

E-Print Network [OSTI]

as a component of the Community Earth System Model (CESM); the computation- ally-modern Glimmer-CISM could need to provide better ice sheet dynamics simu- lations in Earth system models to more accurately

148

The shallow shelf approximation as a "sliding law" in a thermomechanically coupled ice sheet model  

E-Print Network [OSTI]

The shallow shelf approximation is a better ``sliding law'' for ice sheet modeling than those sliding laws in which basal velocity is a function of driving stress. The shallow shelf approximation as formulated by \\emph{Schoof} [2006a] is well-suited to this use. Our new thermomechanically coupled sliding scheme is based on a plasticity assumption about the strength of the saturated till underlying the ice sheet in which the till yield stress is given by a Mohr-Coulomb formula using a modeled pore water pressure. Using this scheme, our prognostic whole ice sheet model has convincing ice streams. Driving stress is balanced in part by membrane stresses, the model is computable at high spatial resolution in parallel, it is stable with respect to parameter changes, and it produces surface velocities seen in actual ice streams.

Bueler, Ed

2008-01-01T23:59:59.000Z

149

The Earth Institute, Columbia University8 annual donor report 2010 9 the ice sheets of antarctica are not  

E-Print Network [OSTI]

The Earth Institute, Columbia University8 annual donor report 2010 9 the ice sheets of antarctica research scientist at the Lamont- Doherty Earth Observatory. In order to model the fate of polar ice sheets cheaply. Secrets Beneath the Ice Experts at the Lamont-Doherty Earth Observatory, including senior

150

Rapid Holocene Deglaciation of the Labrador Sector of the Laurentide Ice Sheet ANDERS E. CARLSON* AND PETER U. CLARK  

E-Print Network [OSTI]

Bay 8.4 cal ka BP (Barber et al. 1999), which caused the LIS to fragment into three ice caps that wereRapid Holocene Deglaciation of the Labrador Sector of the Laurentide Ice Sheet ANDERS E. CARLSON, in final form 31 January 2007) ABSTRACT Retreat of the Laurentide Ice Sheet (LIS) following the Last

Kurapov, Alexander

151

Rapid Holocene Deglaciation of the Labrador Sector of the Laurentide Ice Sheet ANDERS E. CARLSON* AND PETER U. CLARK  

E-Print Network [OSTI]

), which caused the LIS to fragment into three ice caps that were rem- nants of the three originallyRapid Holocene Deglaciation of the Labrador Sector of the Laurentide Ice Sheet ANDERS E. CARLSON, in final form 31 January 2007) ABSTRACT Retreat of the Laurentide Ice Sheet (LIS) following the Last

152

Integrated tephrochronology of the West Antarctic region-Implications for a potential tephra record in the West Antarctic Ice Sheet (WAIS) Divide Ice Core  

E-Print Network [OSTI]

(tephra) and aerosols , produced during major explosive eruptions. Tephra layers in ice cores can provide record in the West Antarctic Ice Sheet (WAIS) Divide Ice Core N.W. Dunbar,1 W.C. McIntosh,1 A.V. Kurbatov@albion.edu) Ice cores from polar regions, in addition to being a climate archives, also capture volcanic particles

Dunbar, Nelia W.

153

Observations of hydroxyl and peroxy radicals and the impact of BrO at Summit, Greenland in 2007 and 2008  

E-Print Network [OSTI]

investigations at Summit, Greenland: An overview, J.upon ice particles in the Greenland snowpack, Geophys. Res.the snowpack at Summit, Greenland, Atmos. Environ. , 36,

2011-01-01T23:59:59.000Z

154

A Bayesian Network for Autonomous Sensor Control during Polar Ice Sheet Measurements  

E-Print Network [OSTI]

of environmental and sensor- related factors. The PRISM sensors are placed on autonomous robotic vehicles ("roversA Bayesian Network for Autonomous Sensor Control during Polar Ice Sheet Measurements Sudha sheets. An important component of PRISM is an intelligent, autonomous Synthetic Aperture Radar that can

Kansas, University of

155

Constraints on the lake volume required for hydro-fracture through ice sheets  

E-Print Network [OSTI]

Constraints on the lake volume required for hydro-fracture through ice sheets M. J. Krawczynski,1 M April 2009; published 16 May 2009. [1] Water-filled cracks are an effective mechanism to drive hydro to rapidly drive hydro-fractures through 1­1.5 km of subfreezing ice. This represents $98% of the meltwater

Skemer, Philip

156

/ 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

157

An update on land-ice modeling in the CESM  

SciTech Connect (OSTI)

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

158

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

159

Time-variable gravity observations of ice sheet mass balance: Precision and limitations of the GRACE satellite data  

E-Print Network [OSTI]

contribution to sea-level rise observed by GRACE withand ice caps to sea level rise, Nature, 482, 514518. King,ice sheets to sea level rise, Geophys. Res. Lett. , 38,

Velicogna, I.; Wahr, J.

2013-01-01T23:59:59.000Z

160

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

Note: This page contains sample records for the topic "greenland ice sheet" 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

rsted Lecture at DTU, 1 November 2013 at 14:00 Mechanics on our planet: Ice sheets,  

E-Print Network [OSTI]

; significant energy in periods between 20 and 100 sec (much longer than for standard earthquakes of similar Ms pendulum period (size scale large); 2. Small gravity drive, water ~ ice; 3. Mélange adds effective mass;Greenland meltwater lake (dark area) (Das et al., Sci., 2008) Early October 2006 SAR image (gray- scale

162

Neglecting ice-atmosphere interactions underestimates ice sheet melt in millennial-scale deglaciation simulations  

E-Print Network [OSTI]

produce an interactive coupled integration: Atmospheric dynamics were equilibrated to an initial iceconstant ice albedos. None of these cases is able to produceproduce substantial deglaciation on a realistic timescale is attributed to the use of temporally invariant ice

Pritchard, M. S.; Bush, A. B.; Marshall, S. J.

2008-01-01T23:59:59.000Z

163

Glaciohydraulic supercooling in former ice sheets? Grahame J. Larson a,*, Daniel E. Lawson b  

E-Print Network [OSTI]

a Department of Geological Sciences, Michigan State University, East Lansing MI 48824, USA b Geophysical Vegas, NV 89154-4010, USA g Department of Geology, Central Michigan University, Mount Pleasant, MI 48859Glaciohydraulic supercooling in former ice sheets? Grahame J. Larson a,*, Daniel E. Lawson b

Lachniet, Matthew S.

164

Quaternary Science Reviews 27 (2008) 941955 Chronological constraints on Cordilleran Ice Sheet glaciomarine  

E-Print Network [OSTI]

,, A.S. Changb a Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109 1005Quaternary Science Reviews 27 (2008) 941955 Chronological constraints on Cordilleran Ice Sheet, USA b School of Earth and Ocean Sciences, University of Victoria, Victoria, BC, Canada Received 12

Pedersen, Tom

2008-01-01T23:59:59.000Z

165

The ablation zone in northeast Greenland: ice types, albedos and impurities  

E-Print Network [OSTI]

), Box 156, NO-9171 Longyearbyen, Norway E-mail: carl.egede.boggild@unis.no 2 Department of Atmospheric Sciences, University of Washington, Seattle, Washington 98195-1640, USA 3 Canadian Forest Service, Northern in the ablation zone (Hanna and others, 2005; Box and others, 2006). The major source of energy for melting ice

Warren, Stephen

166

Development and Applications of the Community Ice Sheet Model  

SciTech Connect (OSTI)

The initial goals of the project are: (1) create a model for land ice that includes relevant and necessary dynamics, physical processes, and couplings; and (2) apply that model to say something more substantial about SLR in Lme for IPCC AR5 (AR6?).

Hoffman, Matthew J. [Los Alamos National Laboratory; Lipscomb, William H. [Los Alamos National Laboratory; Price, Stephen F. [Los Alamos National Laboratory; Johnson, Jesse [University of Montana; Sacks, William [National Center for Atmospheric Research

2012-07-23T23:59:59.000Z

167

Ice cores drilled from lake and ocean floors, continents, and ice sheets provide geoscientists with the most extensive and accurate picture of the earth!s  

E-Print Network [OSTI]

zer Ice cores drilled from lake and ocean floors, continents, and ice sheets provide geoscientists technologies and advanced equipment like high-resolution color line-scanners and multi-sensor data loggers displays run by a single computer all the way down to the new MacBook. Future development will incorporate

Johnson, Andrew

168

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

169

New Method Relates Greenland Ice Sheet Changes to Sea-Level Rise | U.S. DOE  

Office of Science (SC) Website

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr MayAtmosphericNuclear SecurityTensile Strain Switched5 Industrial CarbonArticlesHuman Resources HumanOffice ofNP User

170

Greenland Ice Sheet "Sliding" a Small Contributor to Future Sea-Level  

Office of Science (SC) Website

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr MayAtmosphericNuclear SecurityTensile Strain Switched5 Industrial CarbonArticlesHumanJuneDocumentingFermiGeorge A.Rise | U.S. DOE Office of

171

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

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May JunDatastreamsmmcrcalgovInstrumentsrucLas Conchas recovery challenge fund LasDubeyChallenge Melrose named top team inlevel rise

172

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

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May JunDatastreamsmmcrcalgovInstrumentsrucLas Conchas recovery challenge fund LasDubeyChallenge Melrose named top team inlevel

173

Earth Planets Space, 57, 895902, 2005 Short time-scale heating of the Earth's mantle by ice-sheet dynamics  

E-Print Network [OSTI]

by modeling the linear response of a self-gravitating viscoelastic planet, the gravity field anoma- lies haveEarth Planets Space, 57, 895­902, 2005 Short time-scale heating of the Earth's mantle by ice-scale energy transfer from the ice sheet loading and unloading processes to the Earth's interior via viscous

Hanyk, Ladislav

174

Formation of lobate debris aprons on Mars: Assessment of regional ice sheet collapse and debris-cover armoring  

E-Print Network [OSTI]

not have attained temperatures near or above the ice melting point and retained their current shape, a findFormation of lobate debris aprons on Mars: Assessment of regional ice sheet collapse and debris Keywords: Mars, climate Mars, surface Mars, polar geology Mars, polar caps a b s t r a c t Lobate debris

Marchant, David R.

175

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

E-Print Network [OSTI]

increase of HCl levels (up to 17 ng g?1 ) took place as a result of the setup of waste incineration over the 20th century, likely in relation to waste incineration after 1965. In Greenland snow layers emissions, waste incineration, coal burning 1. Introduction [2] In addition to HNO3 and H2SO4, HCl

Fischer, Hubertus

176

Eurasian ice-sheet interaction in northwestern Russia throughout the late KURT H. KJR, EILIV LARSEN, SVEND FUNDER, IGOR N. DEMIDOV, MARIA JENSEN, LENA HA KANSSON AND  

E-Print Network [OSTI]

U N C O R R EC TED PR O O F Eurasian ice-sheet interaction in northwestern Russia throughout°kansson, L. & Murray, A. 2006 (August): Eurasian ice-sheet interaction in northwestern Russia throughout the Kanin Peninsula and Chyoshskaya Bay in northwestern Russia contain information on the marginal behaviour

Ingólfsson, ?lafur

177

Ice sheets  

E-Print Network [OSTI]

mitigates recent sea-level rise. Science, 308, 1898-1901J. (2004). Accelerated sea-level rise from West Antarctica.and contributions to sea-level rise: 1992-2002. Journal of

Bentley, Charles G.; Thomas, Robert H.; Velicogna, Isabella

2007-01-01T23:59:59.000Z

178

Mapping of Ice Sheet Deep Layers and Fast Outlet Glaciers with Multi-Channel-High-Sensitivity Radar  

E-Print Network [OSTI]

This dissertation discusses the waveform design, the development of SAR and clutter reduction algorithms for MCRDS radars that are developed at CReSIS to map the ice-sheet bed, deep internal layers and fast-flowing outlet glaciers. It is verified...

Li, Jilu

2009-12-29T23:59:59.000Z

179

Measuring Greenland Glacier Dynamics with Remotely Sensed Data  

E-Print Network [OSTI]

Measuring Greenland Glacier Dynamics with Remotely Sensed Data Steve Foga University of Kansas, Geography M.A. Student Photo by: Phil Pasquini The importance of studying glacier ice Study area Difference in ice velocity of Helheim Glacier...

Foga, Steve

2013-01-15T23:59:59.000Z

180

Regional sensitivity of Greenland precipitation to NAO variability E. Mosley-Thompson,1,2  

E-Print Network [OSTI]

Regional sensitivity of Greenland precipitation to NAO variability E. Mosley-Thompson,1,2 C. R, particularly under a warming Earth scenario. As Greenland precipitation is modulated by the NAO, ice core-derived accumulation histories are incorporated into multi-proxy reconstructions. New ice core records from Greenland

Howat, Ian M.

Note: This page contains sample records for the topic "greenland ice sheet" 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

Dynamically coupling the non-linear Stokes equations with the Shallow Ice Approximation in glaciology: Description and first applications of the ISCAL method  

E-Print Network [OSTI]

We propose and implement a new method, called the Ice Sheet Coupled Approximation Levels (ISCAL) method, for simulation of ice sheet flow in large domains under long time-intervals. The method couples the exact, full Stokes (FS) equations with the Shallow Ice Approximation (SIA). The part of the domain where SIA is applied is determined automatically and dynamically based on estimates of the modeling error. For a three dimensional model problem where the number of degrees of freedom is comparable to a real world application, ISCAL performs almost an order of magnitude faster with a low reduction in accuracy compared to a monolithic FS. Furthermore, ISCAL is shown to be able to detect rapid dynamic changes in the flow. Three different error estimations are applied and compared. Finally, ISCAL is applied to the Greenland Ice Sheet, proving ISCAL to be a potential valuable tool for the ice sheet modeling community.

Ahlkrona, Josefin; Kirchner, Nina; Zwinger, Thomas

2015-01-01T23:59:59.000Z

182

COMMUNITY PROFILE Greenland, New Hampshire  

E-Print Network [OSTI]

GREENLAND COMMUNITY PROFILE REPORT Greenland, New Hampshire February 3 & 4, 2006 #12;TABLE......................................................................................................................................3 Creating a Community Profile in Greenland

New Hampshire, University of

183

A new era of sub-millimeter GRB afterglow follow-ups with the Greenland Telescope  

E-Print Network [OSTI]

A planned rapid submillimeter (submm) Gamma Ray Burst (GRBs) follow-up observations conducted using the Greenland Telescope (GLT) is presented. The GLT is a 12-m submm telescope to be located at the top of the Greenland ice sheet, where the high-altitude and dry weather porvides excellent conditions for observations at submm wavelengths. With its combination of wavelength window and rapid responding system, the GLT will explore new insights on GRBs. Summarizing the current achievements of submm GRB follow-ups, we identify the following three scientific goals regarding GRBs: (1) systematic detection of bright submm emissions originating from reverse shock (RS) in the early afterglow phase, (2) characterization of forward shock and RS emissions by capturing their peak flux and frequencies and performing continuous monitoring, and (3) detections of GRBs as a result of the explosion of first-generation stars result of GRBs at a high redshift through systematic rapid follow ups. The light curves and spectra calcul...

Urata, Yuji; Asada, Keiichi; Hirashita, Hiroyuki; Inoue, Makoto; Ho, Paul T P

2015-01-01T23:59:59.000Z

184

OSL ages on glaciofluvial sediment in northern Lower Michigan constrain expansion of the Laurentide ice sheet  

E-Print Network [OSTI]

, Michigan State University, East Lansing, MI 48824-1117, USA b Department of Earth and Environmental for the MIS 2 (late Wisconsin) advance into central northern Lower Michigan. We suggest that widespread ice chronologic control on the advancing MIS 2 ice margin in this part of Lower Michigan and refine the under

Schaetzl, Randall

185

Mapping Greenland's mass loss in space and time Christopher Harig1  

E-Print Network [OSTI]

Mapping Greenland's mass loss in space and time Christopher Harig1 and Frederik J. Simons lost from the Greenland ice cap, based on satellite gravity data collected by the Gravity Recovery distribution of Greenland's mass loss and how the geographical pattern has varied on relatively shorter time

Simons, Frederik J.

186

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

187

A View of Antarctic Ice-Sheet Evolution from Sea-Level and Deep-Sea Isotope Changes During the Late Cretaceous-Cenozoic  

E-Print Network [OSTI]

. Proceedings of the 10th International Symposium on Antarctic Earth Sciences. Washington, DC: The National Academies Press. doi:10.3133/of2007-1047.kp06 A View of Antarctic Ice-Sheet Evolution from Sea-Level and Deep-Sea Isotope Changes During the Late...

Miller, K. G.; Wright, J. D.; Katz, M. E.; Browning, J. V.; Cramer, B. S.; Wade, Bridget S.; Mizintseva, S. F.

2008-01-01T23:59:59.000Z

188

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

189

Glaciers, ice sheets, and sea level: effect of a CO/sub 2/-induced climatic change  

SciTech Connect (OSTI)

The workshop examined the basic questions of how much water has been exchanged between land ice and ocean during the last century, what is happening now, and, given existing climate-modeling prediction, how much exchange can be expected in the next century. In addition, the evidence for exchange was examined and gaps in that evidence were identified. The report includes the 23 presentations made at the workshop, summarizes the workshop discussion, and presents the Committee's findings and recommendations. Separate abstracts have been prepared for the 23 presentations.

none,

1985-09-01T23:59:59.000Z

190

Sources and fate of freshwater exported in the East Greenland Current Paul A. Dodd,1,2  

E-Print Network [OSTI]

Sources and fate of freshwater exported in the East Greenland Current Paul A. Dodd,1,2 Karen J] Monitoring the sources and fate of freshwater in the East Greenland Current (EGC) is important, as this water, with a significant proportion of sea ice drifting into the Nordic Seas or on to the East Greenland Shelf. We conclude

Naveira Garabato, Alberto

191

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

SciTech Connect (OSTI)

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

192

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]

from observations, which show upwelling of dirty, subglacially derived meltwater near the centre of the calving ice front during summer months (Chauch et al., 2013)20 (Fig. 1). The high melt rates are caused by entrainment of warm ambient fjord water... ; Rignot and Kanagaratnam, 2006; Howat et al., 2007), raising con- cerns about its future response to changing global climate and the impact this might have on global sea level. The two factors, which govern this loss, are (1) an overall neg- ative surface...

Todd, J.; Christo?ersen, P.

2014-07-02T23:59:59.000Z

193

115 year ice-core data from Akademii Nauk ice cap, Severnaya Zemlya: high-resolution record of Eurasian Arctic climate change  

E-Print Network [OSTI]

115 year ice-core data from Akademii Nauk ice cap, Severnaya Zemlya: high-resolution record ABSTRACT. From 1999 to 2001 a 724 m deep ice core was drilled on Akademii Nauk ice cap, Severnaya Zemlya Greenland are needed. Therefore, in the Eurasian Arctic several ice cores from ice caps on Svalbard

Fischer, Hubertus

194

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

195

Synoptic Scale Weather Patterns Associated with Annual Snow Accumulation Variability in North-Central Greenland  

E-Print Network [OSTI]

Abstract Previous studies on the synoptic forcing of high elevation areas of central Greenland have mostly relied on ice cores, snow pits, mesoscale models, and climate models. In this study, a radar-measured 118-year annual snow accumulation record...

CHEN, SHU

2013-08-31T23:59:59.000Z

196

Slow retreat of a land based sector of the West Greenland Ice Sheet during the Holocene Thermal Maximum: evidence from threshold  

E-Print Network [OSTI]

of Geology and Mineral Resources Engineering, Norwegian University of Science and Technology, Sem Særlands to the influence of melt water on global sea level rise and potentially on large-scale ocean circulation and thus the global climate system in general (e.g. Alley et al., 2005, 2010; IPCC, 2007). Recent instrumental data

Briner, Jason P.

197

Effect of atmospheric water vapor on modification of stable isotopes in near-surface snow on ice sheets  

E-Print Network [OSTI]

temperature and the abundance of heavy isotopes of water found in water vapor and precipitation as functionsEffect of atmospheric water vapor on modification of stable isotopes in near-surface snow on ice fractionation model is developed to investigate postdepositional modification of stable isotopes of water

Walden, Von P.

198

1, 351383, 2007 Greenland surface  

E-Print Network [OSTI]

TCD 1, 351383, 2007 Greenland surface mass balance at the end of this century G. Krinner and N-resolution simulations of the surface mass balance of Greenland at the end of this century G. Krinner and N. Julien LGGE Correspondence to: G. Krinner (krinner@ujf-grenoble.fr) 351 #12;TCD 1, 351383, 2007 Greenland surface mass

Paris-Sud XI, Universit de

199

Temperature reconstruction at the West Antarctic Ice Sheet Divide, for the last millennium, from the combination of borehole temperature and inert gas isotope measurements /  

E-Print Network [OSTI]

the downward motion of the ice could produce a more detailedanalysis with an ice flow model to produce an accumulationcombined with the ice-albedo feedback may produce a cooling

Orsi, Anais J.

2013-01-01T23:59:59.000Z

200

The satellite gravimetry measurements from GRACE enable analysis of mass changes on Earth, including recent mass loss from ice sheets and glaciers. However, GRACE  

E-Print Network [OSTI]

several large ice caps exist, and a southern part (SCAA), with two large ice caps, many smaller glaciers is positive on the high areas of the ice caps, and negative along most glacier edges. SMB on the tundra in winter that melts again each summer. ICE LOSS Tip: check the video! FINAL NOTES 1. Only now we are able

Utrecht, Universiteit

Note: This page contains sample records for the topic "greenland ice sheet" 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

Investigation of Glacial Dynamics in the Lambert Glacier-Amery Ice Shelf System (LAS) Using Remote Sensing  

E-Print Network [OSTI]

Numerous recent studies have documented dynamic changes in the behaviors of large marine-terminating outlet glaciers and ice streams in Greenland, the Antarctic Peninsula, and West Antarctica. However, fewer observations of outlet glaciers and ice...

Chi, Zhaohui 1982-

2012-12-10T23:59:59.000Z

202

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

203

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

204

Temperature reconstruction at the West Antarctic Ice Sheet Divide, for the last millennium, from the combination of borehole temperature and inert gas isotope measurements /  

E-Print Network [OSTI]

with a global cooling during the Little Ice Age period,with the ice-albedo feedback may produce a cooling signalice, and provide a way to calibrate it. WAIS-Divide experienced a long term cooling

Orsi, Anais J.

2013-01-01T23:59:59.000Z

205

BISICLES Captures Details of Retreating Antarctic Ice  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

suggest that the shrinking West Antarctic ice sheet is contributing to global sea level rise. But until recently, scientists could not accurately model the physical...

206

A geocoding information system for Greenland  

E-Print Network [OSTI]

A geocoding information system for Greenland Janis Siksnans Kongens Lyngby 2012 IMM-MSc-2012-48 #12-XXXX #12;Summary Currently, addressing practices in Greenland do not fully support geocoding. Addressing the current addressing practices in Greenland. Asiaq is a public organization of the Government of Greenland

207

Greenland Meadows LID Case Study: Water Quality  

E-Print Network [OSTI]

Greenland Meadows LID Case Study: Water Quality Greenland Meadows is a retail shopping center built in 2008 by Newton, Mass.- based New England Development in Greenland, N.H. The development is located Development and Community Decisions can be found at http://www.unh.edu/unhsc/ftl/ Greenland Meadows features

208

FEBRUARY 2008|158 THE GREENLAND STIRRING  

E-Print Network [OSTI]

FEBRUARY 2008|158 THE GREENLAND STIRRING ROD: PRESSURE DRAG AND THE ATLANTIC STORM TRACK Greenland of wintertime planetary waves episodically places Greenland in the path of the polar jet stream and associatedwest pressure drag exerted on Greenland's topography. Pressure drag is a key component of the zonal momentum

209

act era proceedings: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

from Greenland ice sheet accumulation: An ERA40 study M. A the Greenland Ice Sheet (GrIS) and large scale circulation patterns, cyclone frequency, and strength. Four climate...

210

XXII ICTAM, 2529 August 2008, Adelaide, Australia EXPERIMENTAL AND THEORETICAL MODELLING OF ICE SHEETSHELF GROUNDING  

E-Print Network [OSTI]

melting of the polar ice caps due to global warming, a dynamical collapse of the ice sheets has the dynamical stability of shelving ice sheets. INTRODUCTION The Antarctic ice cap contains several tensXXII ICTAM, 2529 August 2008, Adelaide, Australia EXPERIMENTAL AND THEORETICAL MODELLING OF ICE

Worster, M. Grae

211

Rapid volume loss from two East Greenland outlet glaciers quantified using repeat stereo satellite imagery  

E-Print Network [OSTI]

[1] The coastal portions of Kangerdlugssuaq and Helheim glaciers in southeast Greenland lost at least 51 8 km3 yr?1 of ice between 20012006 due to thinning and retreat, according to an analysis of sequential digital elevation models (DEMs...

Stearns, Leigh; Hamilton, Gordon S.

2007-03-14T23:59:59.000Z

212

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

213

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

214

View of NY harbor from the JOIDES Resolution! in an ice-free world (73 m rise)!  

E-Print Network [OSTI]

Caps:! Melting land ice adds to ocean volume, but not sea ice! IPCC2001! Alpine! #12;Why Is global sea level Is rising today?! .! Melting mountain glaciers/ice caps ("alpine" and! continental ice sheets error: 20-60 cm (does not include ice sheet melting)! http://www.realclimate.org/images/sealevel_1.jpg

215

Environmental Radioactivity in Greenland in 1981  

E-Print Network [OSTI]

Ris-R-471 v Environmental Radioactivity in Greenland in 1981 A. Aarkrog, Henning Dahlgaard, Elis July 1962 #12;Ris-R-471 ENVIRONMENTAL RADIOACTIVITY IN GREENLAND IN 1981 A. Aarkrog, Henning Dahlgaard. Measurements of fallout radioactivity in Greenland in 1981 are reported. Strontium-90 (and Cesium-137 in most

216

Environmental Radioactivity in Greenland in 1978  

E-Print Network [OSTI]

ft I la 0 0 0 0 Risn-R-405 Environmental Radioactivity in Greenland in 1978 A. Aarkrog, Heinz ENVIRONMENTAL RADIOACTIVITY IN GREENLAND IN 1978 A. Aarkrog, Heinz Hansen and J. Lippert Abstract. Heasureaents of fallout radioactivity in Greenland in 1978 are reported. Strontium-90 (and Cesium-137 in most cases

217

Greenland Meadows LID Case Study: Economics  

E-Print Network [OSTI]

Greenland Meadows LID Case Study: Economics Utilizing an LID approach that featured porous asphalt and a gravel wetland, a cost-competitive drainage system was designed for a large retail development. Greenland in Greenland, N.H. The development is located on a 56-acre parcel and includes three, one-story retail

218

The influence of subglacial hydrology on the flow of West Antarctic ice streams  

E-Print Network [OSTI]

Subglacial hydrology is known to influence the flow of ice. However, difficulty in accessing the base of large ice sheets has made determining the interaction between ice streams, basal sediment and water difficult to discern. The aim of this thesis...

Baker, Narelle Paula Marie

2012-04-10T23:59:59.000Z

219

Bowhead whale springtime song off West Greenland Kathleen M. Stafford  

E-Print Network [OSTI]

Bowhead whale springtime song off West Greenland Kathleen M. Stafford Applied Physics Laboratory 98105 and Greenland Institute of Natural Resources, Box 570, DK-3900 Nuuk, Greenland M. P. Heide-Jrgensen Greenland Institute of Natural Resources, Box 570, DK-3900 Nuuk, Greenland Received 13 February 2008

Laidre, Kristin L.

220

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.

Note: This page contains sample records for the topic "greenland ice sheet" 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

FIRST PRINCIPLES MODELING FOR LIDAR SENSING OF COMPLEX ICE SURFACES  

E-Print Network [OSTI]

FIRST PRINCIPLES MODELING FOR LIDAR SENSING OF COMPLEX ICE SURFACES J. Kerekes, A. Goodenough, S of monitoring the dynamics and mass balance of glaciers, ice caps, and ice sheets. However, it is also known that ice surfaces can have complex 3-dimensional structure, which can challenge their accurate retrieval

Kerekes, John

222

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

223

Recent glacially influenced sedimentary processes on the East Greenland continental slope and deep Greenland Basin  

E-Print Network [OSTI]

Recent glacially influenced sedimentary processes on the East Greenland continental slope and deep Greenland Basin Marga Garca a,*, Julian A. Dowdeswell a , Gemma Ercilla b , Martin Jakobsson c a Scott June 2012 Available online xxx Keywords: Greenland Basin Glacially influenced sedimentary processes

Jakobsson, Martin

224

Melting of small Arctic ice caps observed from ERS scatterometer time series  

E-Print Network [OSTI]

Melting of small Arctic ice caps observed from ERS scatterometer time series Laurence C. Smith,1 of melt onset can be observed over small ice caps, as well as the major ice sheets and multi-year sea ice for 14 small Arctic ice caps from 19922000. Interannual and regional variability in the timing of melt

Smith, Laurence C.

225

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

226

Global Land Ice Measurements from Space Publisher: Springer Praxis Books, Subseries: Geophysical Sciences  

E-Print Network [OSTI]

Global Land Ice Measurements from Space Publisher: Springer Praxis Books, Subseries: Geophysical perceptions about the importance of fluctuations of glaciers and ice sheets (Jeffrey S. Kargel) 1.1Early.2.2. Modern impacts of changing glaciers and ice sheets on people 0.2.3. Recent public perceptions about

227

A metapopulation model for Canadian and West Greenland narwhals  

E-Print Network [OSTI]

A metapopulation model for Canadian and West Greenland narwhals M. P. Heide-Jrgensen1 , P. R. Richard2 , R. Dietz3 & K. L. Laidre4 1 Greenland Institute of Natural Resources, Nuuk, Greenland 2-Jrgensen, Greenland Institute of Natural Resources, Strandgade 91, 3, DK-1016 Copenhagen K, Denmark. Tel: +45 40257943

Laidre, Kristin L.

228

INTRODUCTION Information on the abundance of large whales in Greenland  

E-Print Network [OSTI]

INTRODUCTION Information on the abundance of large whales in Greenland waters, including fin whales surveys were conducted in West Greenland by the Greenland Fisheries Research Institute (m/v Regina Maris when survey conditions are optimal in Greenlandic waters. Between 1983 and 1993, visual aerial surveys

Laidre, Kristin L.

229

Greenland's Pressure Drag and the Atlantic Storm Track THOMAS JUNG  

E-Print Network [OSTI]

Greenland's Pressure Drag and the Atlantic Storm Track THOMAS JUNG European Centre for Medium of Greenland on the Northern Hemisphere wintertime circulation are discussed. Inviscid pressure drag on Greenland's slopes, calculated from reanalysis data, is related to circulation patterns. Greenland lies

230

Radiocarbon Content of CO 2 Respired from High Arctic Tundra in Northwest Greenland  

E-Print Network [OSTI]

J. E. , 2002: Survey of Greenland instrumental temperaturetypes in northwestern Greenland. Arctic, Antarctic, andfen ecosystem in NE-Greenland. Theoretical and Applied

Czimczik, Claudia I; Welker, Jeffrey M

2010-01-01T23:59:59.000Z

231

Persistent multi-decadal Greenland temperature fluctuation through the last millennium  

E-Print Network [OSTI]

Cappelen J (2006) Extending Greenland temper- ature recordssurface elevation at the Greenland summit. J Glaciol 48:199hemisphere tempera- ture and Greenland temperature changed

Kobashi, Takuro; Severinghaus, Jeffrey P.; Barnola, Jean-Marc; Kawamura, Kenji; Carter, Tara; Nakaegawa, Tosiyuki

2010-01-01T23:59:59.000Z

232

A lattice model to simulate ice-structure interaction  

E-Print Network [OSTI]

A lattice model to simulate ice-structure interaction O. Dorival, A. V. Metrikine, A. Simone of Technology P. O. Box 5048, 2600 GA Delft, Netherlands Abstract The interaction between ice sheets, due to the complexity of ice material the use of small-scale experiments is problematic if one aims

Boyer, Edmond

233

Ice shelf-ocean interactions in a general circulation model : melt-rate modulation due to mean flow and tidal currents  

E-Print Network [OSTI]

Interactions between the ocean circulation in sub-ice shelf cavities and the overlying ice shelf have received considerable attention in the context of observed changes in flow speeds of marine ice sheets around Antarctica. ...

Dansereau, Vronique

2012-01-01T23:59:59.000Z

234

Glacial geology and glaciology of the Younger Dryas ice cap in Scotland  

E-Print Network [OSTI]

This thesis uses geological field data and numerical ice sheet modelling to study the Younger Dryas ice cap in Scotland. The Younger Dryas stadial is important because it represents the most recent period of high-magnitude ...

Golledge, Nicholas Robert

2009-01-01T23:59:59.000Z

235

Analysis of glacial earthquakes Victor C. Tsai1  

E-Print Network [OSTI]

, the events cluster into seven regions, all of which correspond to regions of very high ice flow and most, Helheim Glacier, the southeast Greenland glaciers, the northwest Greenland glaciers, Rinks Isbrae that both the Greenland and Antarctic ice sheets are drained by narrow but fast moving features known as ice

Tsai, Victor C.

236

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

237

Pleistocene ice and paleo-strain rates at Taylor Glacier, Antarctica S.M. Aciego a  

E-Print Network [OSTI]

Pleistocene ice and paleo-strain rates at Taylor Glacier, Antarctica S.M. Aciego a , K.M. Cuffey b September 2006 Abstract Ice exposed in ablation zones of ice sheets can be a valuable source of samples for paleoclimate studies and information about long-term ice dynamics. We report a 28-km long stable isotope

Severinghaus, Jeffrey P.

238

Ice-shelf collapse from subsurface warming as a trigger for Heinrich events  

E-Print Network [OSTI]

in Antarctica, the resulting ice-shelf loss and attendant HSIS acceleration would produce a Heinrich eventIce-shelf collapse from subsurface warming as a trigger for Heinrich events Shaun A. Marcotta,1-discharge events from the Hudson Strait Ice Stream (HSIS) of the Laurentide Ice Sheet, referred to as Heinrich

Schmittner, Andreas

239

STATE OF THE CLIMATE Jessica Blunden Derek S. Arndt  

E-Print Network [OSTI]

melting and a negative mass balance. To the west, the mass loss from glaciers and ice caps in the Canadian and ice caps (outside Greenland); Greenland Ice Sheet; Permafrost; Lake ice; Sea ice; Ocean; and Ocean in the dominant wind pat- tern, responding to changes in the polar vortex, which affected the distribution

240

The Role of Snow and Ice in the Climate System  

SciTech Connect (OSTI)

Global snow and ice cover (the 'cryosphere') plays a major role in global climate and hydrology through a range of complex interactions and feedbacks, the best known of which is the ice - albedo feedback. Snow and ice cover undergo marked seasonal and long term changes in extent and thickness. The perennial elements - the major ice sheets and permafrost - play a role in present-day regional and local climate and hydrology, but the large seasonal variations in snow cover and sea ice are of importance on continental to hemispheric scales. The characteristics of these variations, especially in the Northern Hemisphere, and evidence for recent trends in snow and ice extent are discussed.

Barry, Roger (NSIDC) [NSIDC

2007-12-19T23:59:59.000Z

Note: This page contains sample records for the topic "greenland ice sheet" 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

Probing Fukushima with cosmic rays should help speed cleanup...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

cancer, anemia gleaned from ribosome research Complex systems influence melting of Greenland ice sheet Related Articles All Stories Rocket flight test at the Energetic Materials...

242

World's largest single crystal of gold verified by Los Alamos...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

cancer, anemia gleaned from ribosome research Complex systems influence melting of Greenland ice sheet Related Articles All Stories Secure computing for the 'Everyman' goes to...

243

Secure computing for the 'Everyman' goes to market  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

cancer, anemia gleaned from ribosome research Complex systems influence melting of Greenland ice sheet Related Articles All Stories Scientists detect methane levels three times...

244

Dark spaces could change the way we think about galaxies  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

cancer, anemia gleaned from ribosome research Complex systems influence melting of Greenland ice sheet Related Articles All Stories The newly discovered rolling movement shown...

245

acid levels contribute: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

sea level by 7 m. Keywords: sea level; ice sheet; Greenland; Antarctica; climate change 1 Huybrechts, Philippe 7 Contribution of the Active Site Histidine Residues of...

246

Extending Greenland temperature records into the late eighteenth century  

E-Print Network [OSTI]

Extending Greenland temperature records into the late eighteenth century B. M. Vinther,1 K. K records for Greenland reach back to the late nineteenth century at a few sites. Combining early record back to the year 1784. The new extended Greenland temperature record is 9% incomplete. There are

Feigon, Brooke

247

Greenland halibut (Reinhardtius hip-poglossoides (Walbaum)) is a deep-  

E-Print Network [OSTI]

457 Greenland halibut (Reinhardtius hip- poglossoides (Walbaum)) is a deep- water flatfish of high perception of Greenland hali- but as a more free-swimming species than other flatfishes (Merrett and Haedrich. The perception that Greenland hal- ibut may be a pelagically distributed species has primarily been based

248

Late Quaternary history of Washington Land, North Greenland OLE BENNIKE  

E-Print Network [OSTI]

Late Quaternary history of Washington Land, North Greenland OLE BENNIKE Bennike, O. 2002 (September): Late Quaternary history of Washington Land, North Greenland. Boreas, Vol. 31, 260272. Oslo. ISSN 0300-9483. During the last glacial stage, Washington Land in western North Greenland was probably completely inun

Inglfsson, lafur

249

AbstractA total of 7244 Greenland halibut (Reinhardtius hippoglossoides,  

E-Print Network [OSTI]

414 AbstractA total of 7244 Greenland halibut (Reinhardtius hippoglossoides, Walbaum) were tagged in Greenland waters between 1986 and 1998 to in crease information on stock delinea tions, to clarify migration routes, and to describe the seasonal movements of fjord populations. At present 517 recaptured Greenland

250

Epidemiology 69 Sander Greenland and Charles Poole1  

E-Print Network [OSTI]

Epidemiology 69 COMMENTARY Sander Greenland and Charles Poole1 accept that P values are here discussed, for example, by Greenland in 2011).2 The formal view of the P value as a probability conditional of the model). I find Greenland and Poole's1 perspective to be valuable: it is important to go beyond criticism

Gelman, Andrew

251

doi: 10.1130/G32908.1 2012;40;627-630Geology  

E-Print Network [OSTI]

and the effects of Greenland Ice Sheet (GIS) melting on climate over the coming millennium. While some climate., 2009). This sea-level highstand implies substantial melting of the Greenland Ice Sheet (GIS) (Northern the loss of Arctic glaciers and ice caps is included; Otto-Bliesner et al., 2006; Colville et al., 2011

Carlson, Anders

252

Climate Change and National Security  

E-Print Network [OSTI]

Global surface warming (0C) Assumes that the GHG concentration is stabilized at 2000 levelswarming over a long period would melt all of Greenlands ice sheet, raising the global sea level

Alyson, Fleming; Summer, Kelly; Summer, Martin; Lauren, Franck; Jonathan, Mark

2015-01-01T23:59:59.000Z

253

american selected papers: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

DiscussionPaper|DiscussionPaper| Abstract The influence of a reduced Greenland ice sheet (GrIS) on Greenland's surface climate during the Eemian interglacial is studied using a...

254

Antarctic ice sheet fertilises the Southern Ocean  

E-Print Network [OSTI]

Southern Ocean (SO) marine primary productivity (PP) is strongly influenced by the availability of iron in surface waters, which is thought to exert a significant control upon atmospheric CO2 concentrations on glacial/interglacial ...

Death, R.

255

Development of a Seismic Snow Streamer and Use of Multi-Offset Reflection for Determining Glacier Ice Properties  

E-Print Network [OSTI]

Glaciers and ice sheets are important to climate research due to their role in controlling worldwide weather and temperature patterns as well as their potential impact in sea level rise. Because of this, scientists are attempting to model large ice...

Velez Gonzalez, Jose Antonio

2012-12-31T23:59:59.000Z

256

Multiscale modeling of ice deformation behavior M. Montagnata,, O. Castelnaub, P. D. Bonsc, S. H. Fariad,e, O.  

E-Print Network [OSTI]

Multiscale modeling of ice deformation behavior M. Montagnata,, O. Castelnaub, P. D. Bonsc, S. H France (IUF), Paris, France Abstract Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto

Boyer, Edmond

257

SOME CHILLING CONSIDERATIONS ABOUT GLOBAL WARMING  

E-Print Network [OSTI]

;MELTING OF GREENLAND ICE CAP Satellite determination of extent of glacial ice 1992 vs 2002 NASA Arctic Climate Impact Assessment, Cambridge, 2004 Complete melt of the Greenland ice sheet would raise the level over the last thousand years Polar ice cores #12;WHERE IS ALL THIS CO COMING FROM? 2 WHO IS RESPONSIBLE

Schwartz, Stephen E.

258

1, 7797, 2007 Reconstructing the  

E-Print Network [OSTI]

expansion of ocean water, changes in terrestrial storage of water, melting of smaller ice caps and glaciers contribution' the contribution to sea-level change from all glaciers and ice caps outside the large ice sheets of Greenland and Antarctica. Included are the glaciers and ice caps on Greenland and Antarctica which

Paris-Sud XI, Universit de

259

Greenland-Pearl Causal Diagrams 2 November 2009 1 of 16 CAUSAL DIAGRAMS  

E-Print Network [OSTI]

Greenland-Pearl Causal Diagrams 2 November 2009 1 of 16 CAUSAL DIAGRAMS Sander Greenland Department #12;Greenland-Pearl Causal Diagrams 2 November 2009 2 of 16 Introduction From their inception

California at Los Angeles, University of

260

Longpath DOAS observations of surface BrO at Summit, Greenland  

E-Print Network [OSTI]

surface BrO at Summit, Greenland J. Stutz 1 , J. L. Thomasimpact of BrO at Summit, Greenland in 2007 and 2008, Atmos.of peroxy radicals at Summit, Greenland during summer 2003,

2011-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "greenland ice sheet" 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

MEDDELELSER OM GRNLAND BIOSCIENCE 53 2001 Hydroids of Greenland and Iceland  

E-Print Network [OSTI]

MEDDELELSER OM GRNLAND BIOSCIENCE 53 2001 Hydroids of Greenland and Iceland (Cnidaria, Hydrozoa) PETER SCHUCHERT #12;PETER SCHUCHERT. Hydroids of Greenland and Iceland (Cnidaria, Hydrozoa Meddelelser om Grnland Meddelelser om Grnland, which is Danish for Monographs on Greenland, has published

Schuchert, Peter

262

Archimedean Ice  

E-Print Network [OSTI]

The striking boundary dependency (the Arctic Circle phenomenon) exhibited in the ice model on the square lattice extends to other planar set-ups. We present these findings for the triangular and the Kagome lattices. Critical connectivity results guarantee that ice configurations can be generated using the simplest and most efficient local actions. Height functions are utilized throughout the analysis. At the end there is a surprise in store: on the remaining Archimedean lattice for which the ice model can be defined, the 3.4.6.4. lattice, the long range behavior is completely different from the other cases.

Kari Eloranta

2009-09-22T23:59:59.000Z

263

area east greenland: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

schemes and link to the Gateshead Cycling 35 Constraining MODIS snow albedo at large solar zenith angles: Implications for surface energy budget in Greenland Geosciences...

264

Project EARTH-13-RK2: Melting and water drainage from ice-stream margins: theory and computation  

E-Print Network [OSTI]

Project EARTH-13-RK2: Melting and water drainage from ice-stream margins: theory and computation sheets that represent an enormous reservoir of water. The mass of this reservoirs is set by a balance importance. Answers will require a deep understanding of the mechanics of ice sheets, and in particular

Henderson, Gideon

265

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.

266

Fact Sheets  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May JunDatastreamsmmcrcalgovInstrumentsruc DocumentationP-Series toESnet4:Epitaxial ThinFOR IMMEDIATE5FacilitiesFacility willFact Sheets

267

Abundance of narwhals (Monodon monoceros) on the hunting grounds in Greenland  

E-Print Network [OSTI]

Abundance of narwhals (Monodon monoceros) on the hunting grounds in Greenland M. P. HEIDE Greenland Institute of Natural Resources, Bok 570, 3900 Nuuk, Greenland (MPH, KLL, RGH) RUWPA, University to subsistence hunting by Inuit in Greenland and Canada. Scientific advice on the sustainable levels of removals

Laidre, Kristin L.

268

Changes in the Dynamics of Marine-Terminating Outlet Glaciers in West Greenland (2000-2009)  

E-Print Network [OSTI]

Changes in the Dynamics of Marine-Terminating Outlet Glaciers in West Greenland (2000-2009) 1 2 3 of Greenland's marine-terminating outlet glaciers indicate a rapid and complex response to external forcing Greenland's northwestern margin, it is unclear whether west Greenland glaciers have undergone

Howat, Ian M.

269

SOME CHILLING CONSIDERATIONS ABOUT GLOBAL WARMING  

E-Print Network [OSTI]

of Arizona #12;Weiss and Overpeck, University of Arizona #12;MELTING OF GREENLAND ICE CAP Satellite Complete melt of the Greenland ice sheet would raise the level of the global ocean 7 meters. #12 thousand years Polar ice cores #12;GREENHOUSE GAS FORCING AND CHANGE IN GLOBAL MEAN SURFACE TEMPERATURE

Schwartz, Stephen E.

270

Patchogue, New York February 25, 2009  

E-Print Network [OSTI]

, University of Arizona #12;MELTING OF GREENLAND ICE CAP Satellite determination of extent of glacial melt 1992 vs 2002 4002,egdirbmaC,tnemssessAtcapmIetamilCcitcrA Complete melt of the Greenland ice sheet would Polar ice cores #12;GREENHOUSE GAS FORCING AND CHANGE IN GLOBAL MEAN SURFACE TEMPERATURE 1855-2004 -0

Schwartz, Stephen E.

271

CHILLING CONSIDERATIONS GLOBAL WARMING  

E-Print Network [OSTI]

(millionsofsquarekilometers) 30 20 10 MELTING OF GREENLAND ICE CAP Satellite determination of maximum extent of glacial melt Complete melt of the Greenland ice sheet would raise the level of the global ocean 23 feet. ASAN Steffen IS INCREASING Global carbon dioxide concentration over the last thousand years Polar ice cores #12;Mann et al

Schwartz, Stephen E.

272

Greenland New Energy | Open Energy Information  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home Page on Office of Inspector GeneralDepartmentAUDIT REPORTOpen EnergyBoard" form. ToGestionSolar Inc GTSGreenhouseGreenland

273

Fact Sheet Fact Sheet Fact Sheet Fact Sheet Fact Sheet Fact Sheet  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr MayAtmospheric Optical Depth7-1D: Vegetation ProposedUsing ZirconiaPolicy andExsolutionFES6FYRANDOM DRUG TESTING TheMayMarchFact Sheet Fact

274

Fact Sheet Fact Sheet Fact Sheet Fact Sheet Fact Sheet Fact Sheet  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr MayAtmospheric Optical Depth7-1D: Vegetation ProposedUsing ZirconiaPolicy andExsolutionFES6FYRANDOM DRUG TESTING TheMayMarchFact Sheet

275

Fact Sheet Fact Sheet Fact Sheet Fact Sheet Fact Sheet Fact Sheet  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr MayAtmospheric Optical Depth7-1D: Vegetation ProposedUsing ZirconiaPolicy andExsolutionFES6FYRANDOM DRUG TESTING TheMayMarchFact SheetFact

276

Fact Sheet Fact Sheet Fact Sheet Fact Sheet Fact Sheet Fact Sheet  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr MayAtmospheric Optical Depth7-1D: Vegetation ProposedUsing ZirconiaPolicy andExsolutionFES6FYRANDOM DRUG TESTING TheMayMarchFact SheetFact

277

Iced Coffee Iced Yerba Mate "Tea"  

E-Print Network [OSTI]

Iced Coffee Iced Yerba Mate "Tea" Iced Yerba Mate Latte Iced Chai Tea Latte Original, Green Tea Canned Soda Xing Tea Bottled Water Arizona Teas Energy Drinks Red Bull, SF Red Bull & Bing Jones Sodas $0 Cafe au Lait Hot Tea Yerba Mate "Tea" Yerba Mate Latte Chai Tea Latte - Original, Green Tea, or Sugar

278

23 June 2004 Basal Shear Stress of the Ross Ice Streams from Control  

E-Print Network [OSTI]

. Introduction Large areas beneath the West Antarctic Ice Sheet (WAIS) rest on weak unconsolidated sediments.g., unconsolidated sediments) beds, which may have #12;23 June 2004 3 reduced their response time to rapid climate

Macayeal, Douglas R.

279

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

280

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

Note: This page contains sample records for the topic "greenland ice sheet" 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

9 Place-names in north-west Greenland  

E-Print Network [OSTI]

last updated on Monday, 4 April 2011 Accession Form for Individual Recordings: Collection / Collector Name Stephen Leonard Tape No. / Track / Item No. 9 Length of track 23 minutes Title of track Place-names in north-west Greenland Translation...

Leonard, Stephen Pax

282

15 Dorti Peterson life in north-west Greenland  

E-Print Network [OSTI]

last updated on Monday, 4 April 2011 Accession Form for Individual Recordings: Collection / Collector Name Stephen Leonard Tape No. / Track / Item No. 15 Length of track 40 minutes Title of track Dorti Peterson life in north-west Greenland...

Leonard, Stephen Pax

283

Experimental Investigation of Direct Expansion Dynamic Ice-on-coil Storage System Used in Residential Buildings  

E-Print Network [OSTI]

better heat exchanger ability caused by the larger surface of sheet ice, steady and low chilled water temperature was directly extracted from an ice storage tank. The longitudinal and axial fin-added coils improved the COP of the refrigerating unit...

Zheng, M.; Kong, F.; Han, Z.; Liu, W.

2006-01-01T23:59:59.000Z

284

Rangeland Sheet 6 Soil Quality Information Sheet  

E-Print Network [OSTI]

decomposition. Chemically stable organic matter gives soil its dark color and is generally the largest pool. Increasing levels of organic matter promote a higher water- holding capacity, which results in increasedRangeland Sheet 6 Soil Quality Information Sheet Rangeland Soil Quality--Organic Matter USDA

285

A radio air shower surface detector as an extension for IceCube and IceTop  

E-Print Network [OSTI]

The IceCube neutrino detector is built into the Antarctic ice sheet at the South Pole to measure high energy neutrinos. For this, 4800 photomultiplier tubes (PMTs) are being deployed at depths between 1450 and 2450 meters into the ice to measure neutrino induced charged particles like muons. IceTop is a surface air shower detector consisting of 160 Cherenkov ice tanks located on top of IceCube. To extend IceTop, a radio air shower detector could be built to significantly increase the sensitivity at higher shower energies and for inclined showers. As air showers induced by cosmic rays are a major part of the muonic background in IceCube, IceTop is not only an air shower detector, but also a veto to reduce the background in IceCube. Air showers are detectable by radio signals with a radio surface detector. The major emission process is the coherent synchrotron radiation emitted by e+ e- shower particles in the Earths magnetic field (geosynchrotron effect). Simulations of the expected radio signals of air showers are shown. The sensitivity and the energy threshold of different antenna field configurations are estimated.

J. Auffenberg; T. Gaisser; K. Helbing; T. Huege; T. Karg; A. Karle

2007-08-24T23:59:59.000Z

286

Photovoltaics (Fact Sheet)  

SciTech Connect (OSTI)

The fact sheet summarizes the goals and activities of the DOE Solar Energy Technologies Program efforts within its photovoltaics subprogram.

Not Available

2010-09-01T23:59:59.000Z

287

Photovoltaics (Fact Sheet)  

SciTech Connect (OSTI)

The fact sheet summarizes the goals and activities of the DOE Solar Energy Technologies Program efforts within its photovoltaics subprogram.

Not Available

2011-06-01T23:59:59.000Z

288

Systems Integration (Fact Sheet)  

SciTech Connect (OSTI)

The fact sheet summarizes the goals and activities of the DOE Solar Energy Technologies Program efforts within its photovoltaics subprogram.

Not Available

2010-09-01T23:59:59.000Z

289

Gasoline Biodesulfurization Fact Sheet  

Broader source: Energy.gov [DOE]

This petroleum industry fact sheet describes how biodesulfurization can yield lower sulfur gasoline at lower production costs.

290

Sheet1 Page 1  

E-Print Network [OSTI]

Sheet1. WABASH 2012 Participant List. Surname. Given Name. Affiliation. Status. Bisch. Dietmar. Vanderbilt faculty. Nica. Alexandru. Waterloo Univ. faculty.

mdd

2012-09-11T23:59:59.000Z

291

The East Greenland Coastal Current : its structure, variability, and large-scale impact  

E-Print Network [OSTI]

The subtidal circulation of the southeast Greenland shelf is described using a set of high resolution hydrographic and velocity transects occupied in summer 2004. The main feature present is the East Greenland Coastal ...

Sutherland, David A. (David Alan)

2008-01-01T23:59:59.000Z

292

WindSat Polarimetric View of Greenland Peter Gaiser and 1  

E-Print Network [OSTI]

WindSat Polarimetric View of Greenland 1 Li Li, 1 Peter Gaiser and 1 Elizabeth Twarog 1 Remote and observation geometry signatures, particularly over Greenland and Antarctic where the signatures are related-polarimetric microwavr radiometry; WindSat; snow; Greenland I. INTRODUCTION WindSat, launched in January 2003

Long, David G.

293

A numerical ocean circulation model of the Norwegian and Greenland Seas  

E-Print Network [OSTI]

A numerical ocean circulation model of the Norwegian and Greenland Seas DAVID P STEVENS School of the Norwegian and Greenland Seas are investigated using a three-dimensional primitive equation ocean circulation and seasonally varying wind and thermohalme forcing. The connections of the Norwegian and Greenland Seas

Stevens, David

294

A new look at Southeast Greenland barrier winds and katabatic flow G.W.K. Moore  

E-Print Network [OSTI]

1 A new look at Southeast Greenland barrier winds and katabatic flow G.W.K. Moore Department; 2 Abstract: Southern Greenland is characterized by a number of high speed low-level weather systems that are all the result of the interaction of the topography of the Greenland with passing extra

Howat, Ian M.

295

Response of the Greenland-Scotland overflow to changing deep water supply from the Arctic Mediterranean  

E-Print Network [OSTI]

Response of the Greenland-Scotland overflow to changing deep water supply from the Arctic with a topographic barrier is used to study the response of the overflows across the Greenland-Scotland Ridge of the exchanges across the ridge is seen when the supply decreases. Transport variations in the East-Greenland

296

Model simulation of Greenland Sea upper-ocean variability S. Hakkinen,1  

E-Print Network [OSTI]

Model simulation of Greenland Sea upper-ocean variability S. Hakkinen,1 F. Dupont,2 M. Karcher,3-ocean water masses coincides with periods of intense deep-water formation in the Greenland Sea. This paper-ocean properties observed in the Greenland Sea, including very dense, saline water masses in the 1950s, 1960s

Zhang, Jinlun

297

SPATIAL FACTOR ANALYSIS OF STREAM SEDIMENT GEOCHEMISTRY DATA FROM SOUTH GREENLAND  

E-Print Network [OSTI]

SPATIAL FACTOR ANALYSIS OF STREAM SEDIMENT GEOCHEMISTRY DATA FROM SOUTH GREENLAND Allan A. Nielsen1 and Greenland, Thoravej 8, DK-2400 Kbenhavn NV, Denmark. ast@geus.dk SUMMARY This paper describes from South Greenland. Kriged MAF images are compared with kriged images based on varimax rotated

298

Atmospheric circulation and cyclone frequency variations linked to the primary modes of Greenland snow accumulation  

E-Print Network [OSTI]

Atmospheric circulation and cyclone frequency variations linked to the primary modes of Greenland from 34 Greenland firn cores, extending from 1982 to 1996, are used to identify spatial accumulation component, representing west-central Greenland accumulation, is correlated to NAO variability, having

Howat, Ian M.

299

Greenland's Island Rule and the Arctic Ocean circulation by Terrence M. Joyce1,2  

E-Print Network [OSTI]

Greenland's Island Rule and the Arctic Ocean circulation by Terrence M. Joyce1,2 and Andrey made for the flow around Greenland. Godfrey's theory has been extended to permit inclusion of Bering Archipelago in the modeled flow west of Greenland. In both models, the forcing has been applied in a quasi

Joyce, Terrence M.

300

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

E-Print Network [OSTI]

Field Metabolic Rate and PCB Adipose Tissue Deposition Efficiency in East Greenland Polar Bears metabolic rates (FMR) and CB153 deposition efficiencies in East Greenland polar bears. Our simulations Greenland polar bears. Citation: Pavlova V, Nabe-Nielsen J, Dietz R, Svenning J-C, Vorkamp K, et al. (2014

Schierup, Mikkel Heide

Note: This page contains sample records for the topic "greenland ice sheet" 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

Spatial variation in the influence of the North Atlantic Oscillation on precipitation across Greenland  

E-Print Network [OSTI]

Greenland Catherine A. Calder,1 Peter F. Craigmile,1 and Ellen Mosley-Thompson2,3 Received 27 July 2007-derived accumulation records from Greenland have been proposed as proxies for North Atlantic Oscillation (NAO Greenland were found to exhibit the strongest linear association with NAO. In this paper, we expand

Howat, Ian M.

302

Chironomids as indicators of the Holocene climatic and environmental history of two lakes in Northeast Greenland  

E-Print Network [OSTI]

in Northeast Greenland STEFFI SCHMIDT, BERND WAGNER, OLIVER HEIRI, MARTIN KLUG, OLE BENNIKE AND MARTIN MELLES as indicators of the Holocene climatic and environmental history of two lakes in Northeast Greenland. Boreas sequences from arctic lakes on Store Koldewey, an island in Northeast Greenland, were investigated

Bern, Universitt

303

Abstract Southwest Greenland provides wintering grounds for 70% (~460,000) of the northern common  

E-Print Network [OSTI]

Abstract Southwest Greenland provides wintering grounds for 70% (~460,000) of the northern common in the eastern Canadian Arctic and western Greenland (Abraham and Finney 1986; Boertmann et al. 1996; Merkel 2004a). All birds from western Greenland and most Canadian breeders, about 70% (463

304

Upper-air temperatures around Greenland: 19642005 Jason E. Box1,2  

E-Print Network [OSTI]

Upper-air temperatures around Greenland: 19642005 Jason E. Box1,2 and Ariel E. Cohen2 Received 15 of 12h balloon soundings from six sites surrounding Greenland reveal distinct patterns of tropospheric-air temperatures around Greenland: 1964 2005, Geophys. Res. Lett., 33, L12706, doi:10.1029/ 2006GL025723. 1

Howat, Ian M.

305

GEOLOGY, July 2008 539 The origin of the vertical motions of East Greenland is a long-  

E-Print Network [OSTI]

GEOLOGY, July 2008 539 ABSTRACT The origin of the vertical motions of East Greenland is a long uplift in central East Greenland. Because the North Atlantic is rimmed by young glacially carved mountain, Greenland, numerical modeling. INTRODUCTION The coastal landscapes of the fjords of the North Atlantic Ocean

Podladchikov, Yuri

306

Fully corrected estimates of common minke whale abundance in West Greenland in 2007  

E-Print Network [OSTI]

Fully corrected estimates of common minke whale abundance in West Greenland in 2007 M.P. HEIDE West Greenland in August and September 2007. A total of 8,670km of survey effort covered 11 strata SURVEY; SATELLITE TAGGING; WEST GREENLAND minke whales to fully corrected total estimates of abundance

Laidre, Kristin L.

307

Upper ocean T-S variations in the Greenland Sea and their association to climatic conditions  

E-Print Network [OSTI]

Upper ocean T-S variations in the Greenland Sea and their association to climatic conditions Sirpa that the salinity variability in the central Greenland Gyre follows closely the sea level pressure (SLP) fluctuations found along the Greenland Coast, e.g., at Angmagssalik. Corresponding large-scale SLP field

308

FOOD HABITS AND DAILY RATION OF GREENLAND HALIBUT, REINHARDTIUS HIPPOGLOSSOIDES, IN  

E-Print Network [OSTI]

FOOD HABITS AND DAILY RATION OF GREENLAND HALIBUT, REINHARDTIUS HIPPOGLOSSOIDES, IN THE EASTERN BERING SEA M. S. YANG AND P. A. LIVINGSTON1 ABSTRACT This study shows that diet of Greenland halibut varies mainly by depth and size, and that size of prey fish increases as the Greenland halibut increases

309

Neogene overflow of Northern Component Water at the Greenland-Scotland Ridge  

E-Print Network [OSTI]

Neogene overflow of Northern Component Water at the Greenland-Scotland Ridge H. R. Poore Department counterpart Northern Component Water (NCW), across the Greenland-Scotland Ridge (GSR) is thought to have,280 words, 12 figures, 3 tables. Keywords: Northern Component Water; Greenland-Scotland Ridge; Iceland

Samworth, Richard

310

Deep convection in the Irminger Sea forced by the Greenland tip jet  

E-Print Network [OSTI]

Deep convection in the Irminger Sea forced by the Greenland tip jet Robert S. Pickart*, Michael A atmospheric jet known as the Greenland tip jet, which forms periodically in the lee of Cape Farewell, Greenland, and is associated with elevated heat flux and strong wind stress curl. Using a history of tip

Pickart, Robert S.

311

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

E-Print Network [OSTI]

643 Improving the precision of otolith-based age estimates for Greenland halibut (Reinhardtius estimates for Greenland halibut (Reinhardtius hip- poglossoides) have low precision, and there is general and Lyons, 1991). The latter is the primary cause of low pre- cision with Greenland halibut

312

NORTHEASTERN NATURALIST2006 13(1):3538 Sea Lamprey Attached to a Greenland Shark in the  

E-Print Network [OSTI]

NORTHEASTERN NATURALIST2006 13(1):3538 Sea Lamprey Attached to a Greenland Shark in the St fork length, male Somniosus microcephalus (Greenland shark) on 9 October 2004 in Baie St. Pancrace, St observation of a sea lamprey attached to a Somniosus microcephalus (Bloch and Schneider) (Greenland shark

Myers, Ransom A.

313

A Greenland Sea Perspective on the Dynamics of Postconvective Eddies* K. I. C. OLIVER  

E-Print Network [OSTI]

A Greenland Sea Perspective on the Dynamics of Postconvective Eddies* K. I. C. OLIVER School and 2) to provide a theoretical context for recent observations of SCVs in the Greenland Sea hundred days. These findings may explain the observed accumulation and longevity of SCVs at the Greenland

Stevens, David

314

Radar Sounding of Glaciers in Greenland C. Allen, B, Wohletz, and S, Gogineni  

E-Print Network [OSTI]

Radar Sounding of Glaciers in Greenland C. Allen, B, Wohletz, and S, Gogineni The University on several flights over Greenland glaciers during the summer of 1995. The radar data were collected the theory and present results of the homomorphic deconvolution procedure. INTRODUCTION The Greenland

Kansas, University of

315

Natural mortality rate, annual fecundity, and maturity at length for Greenland halibut  

E-Print Network [OSTI]

296 Natural mortality rate, annual fecundity, and maturity at length for Greenland halibut% ma- turity, and the rate of instantaneous natural mortality (M) by using GSI for Greenland halibut Greenland halibut (Reinhardtius hip- poglossoides) life history traits and to correctly assess the status

316

Concentrations and Snow-Atmosphere Fluxes of Reactive Nitrogen at Summit, Greenland  

E-Print Network [OSTI]

1 Concentrations and Snow-Atmosphere Fluxes of Reactive Nitrogen at Summit, Greenland J. W. Munger AT SUMMIT, GREENLAND 2 Abstract. Concentrations and fluxes of NOy (total reactive nitrogen), ozone concentra at Summit, Greenland. Median NOy concentrations declined from 947 ppt in May to 444 ppt by July. NOy fluxes

317

The East Greenland Spill Jet* ROBERT S. PICKART, DANIEL J. TORRES, AND PAULA S. FRATANTONI  

E-Print Network [OSTI]

The East Greenland Spill Jet* ROBERT S. PICKART, DANIEL J. TORRES, AND PAULA S. FRATANTONI Woods Greenland shelf break south of Denmark Strait have revealed an intense, narrow current banked against and entraining ambient water. The current has been named the East Greenland Spill Jet. It resides beneath

Pickart, Robert S.

318

AGE, GROWTH, AND SEXUAL MATURITY OF GREENLAND HALIBUT, REINHARDT/US lHPPOGLOSSOIDES (WALBAUM),  

E-Print Network [OSTI]

AGE, GROWTH, AND SEXUAL MATURITY OF GREENLAND HALIBUT, REINHARDT/US lHPPOGLOSSOIDES (WALBAUM), IN THE CANADIAN NORTHWEST ATLANTIC W. R. BOWERIN01 ABSTRACT Age composition of Greenland halibut, Reinhardtius the slowest throughout the range. Onsetofmaturityoffemale Greenland halibutfrom the Gulfof

319

A New Model to Construct Ice Stream Surface Elevation Profiles and Calculate Contributions to Sea-Level Rise  

E-Print Network [OSTI]

to 21st-Century Sea-Level Rise. Science, 321, 1340; DOI:in the Face of Sea-Level Rise: A Hybrid Modeling Approachof ice sheets to sea-level rise. Bibliography Alcamo, J. et

Adachi, Yosuke

2012-01-01T23:59:59.000Z

320

Arctic ice islands  

SciTech Connect (OSTI)

The development of offshore oil and gas resources in the Arctic waters of Alaska requires offshore structures which successfully resist the lateral forces due to moving, drifting ice. Ice islands are floating, a tabular icebergs, up to 60 meters thick, of solid ice throughout their thickness. The ice islands are thus regarded as the strongest ice features in the Arctic; fixed offshore structures which can directly withstand the impact of ice islands are possible but in some locations may be so expensive as to make oilfield development uneconomic. The resolution of the ice island problem requires two research steps: (1) calculation of the probability of interaction between an ice island and an offshore structure in a given region; and (2) if the probability if sufficiently large, then the study of possible interactions between ice island and structure, to discover mitigative measures to deal with the moving ice island. The ice island research conducted during the 1983-1988 interval, which is summarized in this report, was concerned with the first step. Monte Carlo simulations of ice island generation and movement suggest that ice island lifetimes range from 0 to 70 years, and that 85% of the lifetimes are less then 35 years. The simulation shows a mean value of 18 ice islands present at any time in the Arctic Ocean, with a 90% probability of less than 30 ice islands. At this time, approximately 34 ice islands are known, from observations, to exist in the Arctic Ocean, not including the 10-meter thick class of ice islands. Return interval plots from the simulation show that coastal zones of the Beaufort and Chukchi Seas, already leased for oil development, have ice island recurrences of 10 to 100 years. This implies that the ice island hazard must be considered thoroughly, and appropriate safety measures adopted, when offshore oil production plans are formulated for the Alaskan Arctic offshore. 132 refs., 161 figs., 17 tabs.

Sackinger, W.M.; Jeffries, M.O.; Lu, M.C.; Li, F.C.

1988-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "greenland ice sheet" 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

No Confinement Needed: Observation of a Metastable Hydrophobic Wetting Two-Layer Ice on Graphene  

SciTech Connect (OSTI)

The structure of water at interfaces is crucial for processes ranging from photocatalysis to protein folding. Here, we investigate the structure and lattice dynamics of two-layer crystalline ice films grown on a hydrophobic substrate - graphene on Pt(111) - with low energy electron diffraction, reflection-absorption infrared spectroscopy, rare-gas adsorption/desorption, and ab-initio molecular dynamics. Unlike hexagonal ice, which consists of stacks of puckered hexagonal "bilayers", this new ice polymorph consists of two flat hexagonal sheets of water molecules in which the hexagons in each sheet are stacked directly on top of each other. Such two-layer ices have been predicted for water confined between hydrophobic slits, but not previously observed. Our results show that the two-layer ice forms even at zero pressure at a single hydrophobic interface by maximizing the number of hydrogen bonds at the expense of adopting a non-tetrahedral geometry with weakened bonds.

Kimmel, Gregory A.; Matthiesen, Jesper; Baer, Marcel; Mundy, Christopher J.; Petrik, Nikolay G.; Smith, R. Scott; Dohnalek, Zdenek; Kay, Bruce D.

2009-09-09T23:59:59.000Z

322

Fact Sheet LANS PNOV  

Office of Environmental Management (EM)

Fact Sheet NNSA issues Preliminary Notice of Violation to Los Alamos National Security, LLC, for Radiation Protection Violations On April 15, 2011, the National Nuclear Security...

323

Market Acceleration (Fact Sheet)  

SciTech Connect (OSTI)

The fact sheet summarizes the goals and activities of the DOE Solar Energy Technologies Program efforts within its market acceleration subprogram.

Not Available

2010-09-01T23:59:59.000Z

324

Clean Cities Fact Sheet  

SciTech Connect (OSTI)

This is a routine revision of a general fact sheet that describes the Clean Cities partnership efforts and includes a list of Clean Cities coordinators.

Not Available

2005-09-01T23:59:59.000Z

325

Ice electrode electrolytic cell  

DOE Patents [OSTI]

This invention relates to a method and apparatus for removing heavy metals from waste water, soils, or process streams by electrolytic cell means. The method includes cooling a cell cathode to form an ice layer over the cathode and then applying an electric current to deposit a layer of the heavy metal over the ice. The metal is then easily removed after melting the ice. In a second embodiment, the same ice-covered electrode can be employed to form powdered metals.

Glenn, David F. (Idaho Falls, ID); Suciu, Dan F. (Idaho Falls, ID); Harris, Taryl L. (Idaho Falls, ID); Ingram, Jani C. (Idaho Falls, ID)

1993-01-01T23:59:59.000Z

326

Ice electrode electrolytic cell  

DOE Patents [OSTI]

This invention relates to a method and apparatus for removing heavy metals from waste water, soils, or process streams by electrolytic cell means. The method includes cooling a cell cathode to form an ice layer over the cathode and then applying an electric current to deposit a layer of the heavy metal over the ice. The metal is then easily removed after melting the ice. In a second embodiment, the same ice-covered electrode can be employed to form powdered metals.

Glenn, D.F.; Suciu, D.F.; Harris, T.L.; Ingram, J.C.

1993-04-06T23:59:59.000Z

327

The historical global sea-level budget J.C. MOORE,1,2  

E-Print Network [OSTI]

-level contributions from glaciers and small ice caps, the Greenland ice sheet and thermosteric sea level are available unsurveyed high-latitude small glaciers and ice caps. The sea-level budget from 1850 is estimated using because it takes $50 times more energy to raise sea level by ocean heating than by ice melting (Trenberth

Moore, John

328

The Cryosphere, 1, 5965, 2007 www.the-cryosphere.net/1/59/2007/  

E-Print Network [OSTI]

). Thermal expansion of ocean water, changes in terrestrial storage of water, melting of smaller ice caps by "glacier contribu- tion" the contribution to sea-level change from all glaciers and ice caps outside the large ice sheets of Greenland and Antarctica. Included are the glaciers and ice caps on Green- land

Paris-Sud XI, Universit de

329

Frequently Asked Questions Frequently Asked Question 4.1  

E-Print Network [OSTI]

and contribut- ing to sea level rise. The total contribution of glacier, ice cap and ice sheet melt to sea level of near- balance around 1970, this was followed by increased shrinkage. Melting of glaciers and ice caps and increased Greenland surface melting. Ice interacts with the surrounding climate in complex ways, so

330

A realistic freshwater forcing protocol for ocean-coupled climate models J. van den Berk a,  

E-Print Network [OSTI]

a b s t r a c t A high-end scenario of polar ice loss from the Greenland and Antarctic ice sheet is presented with sepa- rate projections for different mass-loss sites up to the year 2100. For each large ice through melt of drifting ice- bergs. The location and relative magnitude of freshwater forcing due

331

Controversies Regarding the Holocene Sea-Level History of the Northwestern Gulf of Mexico  

E-Print Network [OSTI]

islands, deltas, etc. Glacio-Hydro-Isostatic Models Rheology wrong? Ice sheet ½ size of Greenland grew and Rink, 2008 #12;Winds #12;Wind and Sedimentation Troiani, Simms, et al., in press #12;Paleowinds Troiani

California at Santa Barbara, University of

332

1  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (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...

333

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

Broader source: All U.S. Department of Energy (DOE) Office Webpages (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...

334

1 JANUARY 2004 21T O N I A Z Z O E T A L . 2004 American Meteorological Society  

E-Print Network [OSTI]

with preindustrial atmospheric greenhouse gas composition and with the Greenland ice sheet removed. Two separate pressure center that forces cyclone systems (and hence precipitation) to skirt along its sides with little

Huybrechts, Philippe

335

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

336

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

337

Microcomponent sheet architecture  

DOE Patents [OSTI]

The invention is a microcomponent sheet architecture wherein macroscale unit processes are performed by microscale components. The sheet architecture may be a single laminate with a plurality of separate microcomponent sections or the sheet architecture may be a plurality of laminates with one or more microcomponent sections on each laminate. Each microcomponent or plurality of like microcomponents perform at least one unit operation. A first laminate having a plurality of like first microcomponents is combined with at least a second laminate having a plurality of like second microcomponents thereby combining at least two unit operations to achieve a system operation. 14 figs.

Wegeng, R.S.; Drost, M.K..; McDonald, C.E.

1997-03-18T23:59:59.000Z

338

Microcomponent sheet architecture  

DOE Patents [OSTI]

The invention is a microcomponent sheet architecture wherein macroscale unit processes are performed by microscale components. The sheet architecture may be a single laminate with a plurality of separate microcomponent sections or the sheet architecture may be a plurality of laminates with one or more microcomponent sections on each laminate. Each microcomponent or plurality of like microcomponents perform at least one unit operation. A first laminate having a plurality of like first microcomponents is combined with at least a second laminate having a plurality of like second microcomponents thereby combining at least two unit operations to achieve a system operation.

Wegeng, Robert S. (Richland, WA); Drost, M. Kevin (Richland, WA); McDonald, Carolyn E. (Richland, WA)

1997-01-01T23:59:59.000Z

339

Predicting Land-Ice Retreat and Sea-Level Rise with the Community Earth System Model  

SciTech Connect (OSTI)

Coastal stakeholders need defensible predictions of 21st century sea-level rise (SLR). IPCC assessments suggest 21st century SLR of {approx}0.5 m under aggressive emission scenarios. Semi-empirical models project SLR of {approx}1 m or more by 2100. Although some sea-level contributions are fairly well constrained by models, others are highly uncertain. Recent studies suggest a potential large contribution ({approx}0.5 m/century) from the marine-based West Antarctic Ice Sheet, linked to changes in Southern Ocean wind stress. To assess the likelihood of fast retreat of marine ice sheets, we need coupled ice-sheet/ocean models that do not yet exist (but are well under way). CESM is uniquely positioned to provide integrated, physics based sea-level predictions.

Lipscomb, William [Los Alamos National Laboratory

2012-06-19T23:59:59.000Z

340

Conventional Hydropower Technologies (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet describes the DOE Water Power Program's conventional hydropower research and development efforts.

Not Available

2011-07-01T23:59:59.000Z

Note: This page contains sample records for the topic "greenland ice sheet" 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.


341

Community Wind Benefits (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet explores the benefits of community wind projects, including citations to published research.

Not Available

2012-11-01T23:59:59.000Z

342

STEP Intern Reference Check Sheet  

Broader source: Energy.gov [DOE]

STEP Intern Reference Check Sheet, from the Tool Kit Framework: Small Town University Energy Program (STEP).

343

Amundsen Sea sea-ice variability, atmospheric circulation, and spatial variations in snow isotopic composition from new West Antarctic firn cores  

E-Print Network [OSTI]

Recent work has documented dramatic changes in the West Antarctic Ice Sheet (WAIS) over the past 30 years (e.g., mass loss, glacier acceleration, surface warming) due largely to the influence of the marine environment. ...

Criscitiello, Alison Sara

2014-01-01T23:59:59.000Z

344

antarctic ice sheet: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Engineering Websites Summary: is a geophysically - and in an age of growing concern about global warming, geopolitically - important portion of Earth. The composition and dynamics...

345

antarctic ice sheets: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Engineering Websites Summary: is a geophysically - and in an age of growing concern about global warming, geopolitically - important portion of Earth. The composition and dynamics...

346

Sandia National Laboratories: Ice-Sheet Simulation Code Matures, Leveraging  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr MayAtmosphericNuclear Security Administration the1 -theErik Spoerke SSLS Exhibit atVehicle Technologies OnAnalysisIEAIMMISGAN

347

Technical Fact Sheets  

Broader source: Energy.gov [DOE]

Technical Fact Sheets (TFS) provide summary-level information on the impact of new, deployed, applied, and/or planned technical approaches supporting EM cleanup projects. The TFS is presented as a...

348

Avian Fact Sheet  

SciTech Connect (OSTI)

OAK-B135 After conducting four national research meetings, producing a document guiding research: Metrics and Methods for Determining or Monitoring Potential Impacts on Birds at Existing and Proposed Wind Energy Sites, 1999, and another paper, Avian Collisions with Wind Turbines: A Summary of Existing Studies and Comparisons to Other Sources of Avian Collision Mortality in the United States, 2001, the subcommittee recognized a need to summarize in a short fact sheet what is known about avian-wind interaction and what questions remain. This fact sheet attempts to summarize in lay terms the result of extensive discussion about avian-wind interaction on land. This fact sheet does not address research conducted on offshore development. This fact sheet is not intended as a conclusion on the subject; rather, it is a summary as of Fall/Winter 2002.

NWCC Wildlife Work Group

2004-12-01T23:59:59.000Z

349

Fact Sheet HEALTH SCIENCE  

E-Print Network [OSTI]

· Long Term Care Administrator · Training Coordinator · Clinical Health Education Specialist · Health Media Director · Long Term Care Facilities Manager Fact Sheet HEALTH SCIENCE Highlights · Health Science

Su, Xiao

350

Energy information sheets  

SciTech Connect (OSTI)

The National Energy Information Center (NEIC), as part of its mission, provides energy information and referral assistance to Federal, State, and local governments, the academic community, business and industrial organizations, and the public. The Energy Information Sheets was developed to provide general information on various aspects of fuel production, prices, consumption, and capability. Additional information on related subject matter can be found in other Energy Information Administration (EIA) publications as referenced at the end of each sheet.

NONE

1995-07-01T23:59:59.000Z

351

Biodiesel Basics (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet provides a brief introduction to biodiesel, including a discussion of biodiesel blends, which blends are best for which vehicles, where to buy biodiesel, how biodiesel compares to diesel fuel in terms of performance, how biodiesel performs in cold weather, whether biodiesel use will plug vehicle filters, how long-term biodiesel use may affect engines, biodiesel fuel standards, and whether biodiesel burns cleaner than diesel fuel. The fact sheet also dismisses the use of vegetable oil as a motor fuel.

Not Available

2014-06-01T23:59:59.000Z

352

Mobile Ice Nucleus Spectrometer  

SciTech Connect (OSTI)

This first year report presents results from a computational fluid dynamics (CFD) study to assess the flow and temperature profiles within the mobile ice nucleus spectrometer.

Kulkarni, Gourihar R.; Kok, G. L.

2012-05-07T23:59:59.000Z

353

Ice Drilling Gallonmilkjugs  

E-Print Network [OSTI]

Ice Drilling Materials · Gallonmilkjugs · Syringes,largeand small · Pitchers · Spraybottles · 13x9? ·Isitbettertosquirtthewaterslowlyorasquicklyaspossible? ·Doestherateatwhichyousquirtthewaterchangethediameteroftheholes? ·Doesthetypeof`drill

Saffman, Mark

354

Material Safety Data Sheets | Department of Energy  

Broader source: Energy.gov (indexed) [DOE]

Material Safety Data Sheets Material Safety Data Sheets Material Safety Data Sheets (MSDSs) provide workers and emergency personnel with ways for handling and working with a...

355

Technology Fact Sheets | Department of Energy  

Energy Savers [EERE]

Fact Sheets Technology Fact Sheets This page contains links to fact sheets describing solid-state lighting, its characteristics, applications, and issues relating to its successful...

356

Fact Sheet: Better Buildings Residential Network | Department...  

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

Fact Sheet: Better Buildings Residential Network Fact Sheet: Better Buildings Residential Network Fact Sheet: Better Buildings Residential Network, increasing the number of...

357

Upton, Long Island, New York April 4, 2011  

E-Print Network [OSTI]

Increase Mote et al., 2005 #12;MELTING OF GREENLAND ICE CAP Satellite determination of maximum extent of glacial melt Complete melt of the Greenland ice sheet would raise the level of the global ocean 23 feet thousand years Polar ice cores #12;GLOBAL ANNUAL TEMPERATURE ANOMALY, 1880-2010 0.8 0.6 0.4 0.2 0.0 -0.2 -0

Schwartz, Stephen E.

358

A TEX86 lake record suggests simultaneous shifts in temperature in Central Europe and Greenland during the last deglaciation  

E-Print Network [OSTI]

A TEX86 lake record suggests simultaneous shifts in temperature in Central Europe and Greenland years. The remarkable resemblance with the Greenland and regional stable oxygen isotope records suggests and Greenland during the last deglaciation, Geophys. Res. Lett., 40, 948953, doi:10.1002/grl.50181. 1

Wehrli, Bernhard

359

A case study of a Greenland lee cyclogenesis event and the subsequent spawning of a tip jet  

E-Print Network [OSTI]

A case study of a Greenland lee cyclogenesis event and the subsequent spawning of a tip jet Carling: With elevations exceeding 2000m in height, Greenland's southern tip acts as a large barrier to storm systems traversing the North Atlantic. As a result of the interaction with Greenland, low-pressure systems located

Pickart, Robert S.

360

P. Schuchert 2001a. Hydroids of Greenland and Iceland (Cnidaria, Hydrozoa). Meddelelser om Grnland 53: 1-184.  

E-Print Network [OSTI]

P. Schuchert 2001a. Hydroids of Greenland and Iceland (Cnidaria, Hydrozoa). Meddelelser om Grnland Kramp (1949) page 42: the existence of the Greenlandic species Zyzzyzus robustus Petersen, 1990 was only noted after the typesetting of the manuscript. page 46: section Distribution: "esatern Greenland" should

Schuchert, Peter

Note: This page contains sample records for the topic "greenland ice sheet" 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

Climatological conditions for the subpolar North Atlantic during the field campaign of the Greenland Flow Distortion Experiment  

E-Print Network [OSTI]

of the Greenland Flow Distortion Experiment G.W.K. Moore Department of Physics University of Toronto R.S. Pickart January 21, 2009 #12; 2 Abstract: Due to its high topography, Greenland results in significant to help document this flow distortion as part of the international research project called the Greenland

Pickart, Robert S.

362

Appendix S1 -A greener Greenland? Normand et al. Appendix S1: Study species and species occurrence data  

E-Print Network [OSTI]

Appendix S1 - A greener Greenland? Normand et al. 1 Appendix S1: Study species and species as in one or several of the floristic provinces bordering Greenland (Fig. S1.1). The selection were based subspecies) was considered. The selected species were assigned maximum heights and Greenlandic species

Zimmermann, Niklaus E.

363

Reionization on ice  

E-Print Network [OSTI]

The case for substantial far infrared ice emission in local ultraluminous infrared galaxies, expected based on the presence of mid-infrared ice absorption in their spectra and the known far infrared optical properties of ice, is still largely unsupported by direct observation owing to insufficient far infrared spectral coverage. Some marginal supportive evidence is presented here. A clear consequence of far infrared ice emission is the need to extend the range of redshifts considered for submillimeter sources. This is demonstrated via the example of HDF 850.1. The solid phase of the ISM during reionization may be dominated by ice, and this could lead to the presence of reionization sources in submillimeter source catalogs. Submillimeter sources not detected at 24 micron in the GOODS-N field are examined. Two candidate reionization sources are identified at 3.6 micron through possible Gunn-Peterson saturation in the Z band.

C. C. Dudley; M. Imanishi; P. R. Maloney

2006-02-15T23:59:59.000Z

364

Constraining MODIS snow albedo at large solar zenith angles: Implications for surface energy budget in Greenland  

E-Print Network [OSTI]

Constraining MODIS snow albedo at large solar zenith angles: Implications for surface energy budget; Solar Zenith Angle; Greenland; Surface Energy Budget 2 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 plays a pivotal role in determining the surface energy balance of Greenland which, by virtue of its area

Zender, Charles

365

Very ice rich permafrost Moderately ice rich permafrost  

E-Print Network [OSTI]

TK lake Very ice rich permafrost Permafrost forest Moderately ice rich permafrost Open Bog Open Fen characteristics (mainly ice content) and burn severity determine trajectories of ecosystem succession post in the presence of moderately ice rich permafrost but have high resilience only under low burn severity in very

Ruess, Roger W.

366

Ice Cream with a Heart Create a new Clemson Ice  

E-Print Network [OSTI]

Ice Cream with a Heart Contest! Create a new Clemson Ice Cream flavor! Raise money for your favorite charity! Win a free Clemson Ice Cream party for your organization! Enter at www organizations. The contest is called Ice Cream with a Heart and its purpose is to help student organizations

Duchowski, Andrew T.

367

Toolbox Safety Talk Safety Data Sheets (SDS)  

E-Print Network [OSTI]

Toolbox Safety Talk Safety Data Sheets (SDS) Environmental Health & Safety Facilities Safety-in sheet to Environmental Health & Safety for recordkeeping. Chemical manufacturers are required to produce Safety Data Sheets (SDS) for all chemicals produced. "Safety Data Sheets", previously referred

Pawlowski, Wojtek

368

Energy information sheets  

SciTech Connect (OSTI)

The National Energy Information Center (NEIC), as part of its mission, provides energy information and referral assistance to Federal, State, and local governments, the academic community, business and industrial organizations, and the general public. Written for the general public, the EIA publication Energy Information Sheets was developed to provide information on various aspects of fuel production, prices, consumption and capability. The information contained herein pertains to energy data as of December 1991. Additional information on related subject matter can be found in other EIA publications as referenced at the end of each sheet.

Not Available

1993-12-02T23:59:59.000Z

369

Accelerating Clean Energy Adoption (Fact Sheet), Weatherization...  

Broader source: Energy.gov (indexed) [DOE]

Accelerating Clean Energy Adoption (Fact Sheet), Weatherization and Intergovernmental Program (WIP) Accelerating Clean Energy Adoption (Fact Sheet), Weatherization and...

370

Home Energy Professional Certifications (Fact Sheet), Guidelines...  

Broader source: Energy.gov (indexed) [DOE]

Certifications (Fact Sheet), Guidelines For Home Energy Professionals, Energy Efficiency & Renewable Energy (EERE) Home Energy Professional Certifications (Fact Sheet),...

371

Clean Domestic Power (Fact Sheet)  

SciTech Connect (OSTI)

This two-page fact sheet describes the priorities and activities of the EERE Geothermal Technologies Program.

Not Available

2010-06-01T23:59:59.000Z

372

Sample Residential Program Term Sheet  

Broader source: Energy.gov (indexed) [DOE]

Goal DRAFT U.S. DOE Sample Residential Program Term Sheet - DRAFT Introduction is seeking to develop an energy...

373

Neglecting ice-atmosphere interactions underestimates ice sheet melt in millennial-scale deglaciation simulations  

E-Print Network [OSTI]

Pergamon Press, New York. Peltier, W. R. (1985), The LAGEOSWu, P. , and W. R. Peltier (1982), Viscous gravitationalmodel based on Wu and Peltier [1982] and Peltier [1985]. A

Pritchard, M. S.; Bush, A. B.; Marshall, S. J.

2008-01-01T23:59:59.000Z

374

Ethanol Basics (Fact Sheet)  

SciTech Connect (OSTI)

Ethanol is a widely-used, domestically-produced renewable fuel made from corn and other plant materials. More than 96% of gasoline sold in the United States contains ethanol. Learn more about this alternative fuel in the Ethanol Basics Fact Sheet, produced by the U.S. Department of Energy's Clean Cities program.

Not Available

2015-01-01T23:59:59.000Z

375

Materials Safety Data Sheets  

E-Print Network [OSTI]

Materials Safety Data Sheets (MSDS) MSDS contain chemical hazard information about substances compounds and solvents. MSDS data can be accessed from the following URLs http://www.ehs.umass.edu/ http://www.chem.umass.edu/Safety the "Important Safety Sites for the University" link to reach a variety of safety related information, including

Schweik, Charles M.

376

Participant Guide Cover Sheet  

E-Print Network [OSTI]

Proposal Management ­ State Transition (diagram) 4 Page 2 #12;eRPM Workflow eRPM system workflow starts Management - State Transitions Page 4 #12;Proposal Management Reviewer Participant Guide Last updated: 03Proposal Management Reviewer Participant Guide Cover Sheet Last updated: 03/20/09 1 of 1 http

Shyy, Wei

377

DOI: 10.1126/science.1118152 , 990 (2006);311Science  

E-Print Network [OSTI]

to enhanced surface meltwater production penetrating to the bed to lubricate its motion (20), and ice-shelf removal (13), ice-front retreat, and glacier ungrounding (21, 22) that reduce resistance to flow- rent models used to project the contribution to sea level from the Greenland Ice Sheet in a changing

Lynch, Michael

378

This chapter describes observations of continuing change in the Arctic environmental system. It is or-  

E-Print Network [OSTI]

for the longest period and largest area of ice sheet melt since at least 1978, and the highest melt rate since in the Canadian Arctic, where the rate of mass loss from small glaciers and ice caps continued to increase system. It is or- ganized into five broad sections: atmosphere, ocean, sea ice cover, land, and Greenland

Bhatt, Uma

379

J. Blunden, D. S. Arndt, and M. O. Baringer, Eds. Associate Eds. K. M.Willett,A. J. Dolman, B. D. Hall, P.W.Thorne, J. M. Levy, H. J. Diamond,  

E-Print Network [OSTI]

. The warm air from the south was responsible for the longest period and largest area of ice sheet melt since small glaciers and ice caps continued to increase. At the circum-Arctic scale, with the exception, ocean, sea ice cover, land, and Greenland. The land section includes vegetation, permafrost, river

380

DIFFRACTION STUDIES OF ICE Alexe BOSAK  

E-Print Network [OSTI]

Ic 28o halo observed at least 7 times since 1629 octahedral particles of ice Ic! #12;Cooling downDIFFRACTION STUDIES OF ICE Alexeï BOSAK European Synchrotron Radiation Facility #12;Ice as the mild threat ice Ih the only ice in the crust #12;Ice as the absolute weapon Ice IX : melting point 45.8°C

Titov, Anatoly

Note: This page contains sample records for the topic "greenland ice sheet" 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.


381

An Attracting Jormungand Climate State for an Energy Balance Model with Ice Line Coupling  

E-Print Network [OSTI]

evidence exists indicating continental ice sheets flowed into the ocean near the equator during. A planet is warmed by incoming solar radiation (or insolation), while it loses heat energy through the emission of outgoing longwave radiation (OLR) to space. The extent to which the surface and clouds reflect

Wilmer, Elizabeth

382

Ice Formation in Gas-Diffusion Layers  

E-Print Network [OSTI]

the University of California. Ice Formation in Gas-Diffusionsub-freezing conditions, ice forms in the gas-diffusionstrategies exist to prevent ice formation, there is little

Dursch, Thomas

2013-01-01T23:59:59.000Z

383

ICE Raids: Compounding Production, Contradiction, and Capitalism  

E-Print Network [OSTI]

America: Factories and ICE Raids Produce Citizens Americansubjects. ICE raids (re)produce workers contradictoryfactories and ICE raids have come to produce immigrant

Reas, Elizabeth I

2009-01-01T23:59:59.000Z

384

Biomolecular Science (Fact Sheet)  

SciTech Connect (OSTI)

A brief fact sheet about NREL Photobiology and Biomolecular Science. The research goal of NREL's Biomolecular Science is to enable cost-competitive advanced lignocellulosic biofuels production by understanding the science critical for overcoming biomass recalcitrance and developing new product and product intermediate pathways. NREL's Photobiology focuses on understanding the capture of solar energy in photosynthetic systems and its use in converting carbon dioxide and water directly into hydrogen and advanced biofuels.

Not Available

2012-04-01T23:59:59.000Z

385

LM FUSRAP Program Fact Sheet | Department of Energy  

Broader source: Energy.gov (indexed) [DOE]

FUSRAP Program Fact Sheet LM FUSRAP Program Fact Sheet LM FUSRAP Program Fact Sheet LM FUSRAP Program Fact Sheet More Documents & Publications FUSRAP Stakeholder Report Overview of...

386

Designing for effective stationkeeping in ice  

E-Print Network [OSTI]

and intervention vessels for Arctic oil and gas. #12;2. An effective Ice Management system · Ice Management for the CIVArctic vessel. - Comparison with the ice model tests carried out in the Aker Arctic ice tank in May 2011

Nørvåg, Kjetil

387

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

388

Schneider Electric ESCO Qualification Sheet  

Broader source: Energy.gov [DOE]

Fact sheet outlines the energy service company (ESCO) qualifications for Schneider Electric in relation to the U.S. Department of Energy's (DOEs) energy savings performance contracts (ESPC).

389

Wind Energy Benefits (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet outlines the top 10 benefits of wind energy, including cost, water savings, job creation, indigenous resource, and low operating costs.

Not Available

2015-01-01T23:59:59.000Z

390

Lockheed Martin ESCO Qualification Sheet  

Broader source: Energy.gov [DOE]

Document outlines the energy service company (ESCO) qualifications sheet for Lockheed Martin under the Department of Energy's (DOEs) energy savings performance contract (ESPC).

391

Secure Data Center (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet describes the purpose, lab specifications, applications scenarios, and information on how to partner with NREL's Secure Data Center at the Energy Systems Integration Facility.

Not Available

2012-08-01T23:59:59.000Z

392

MEAT, POULTRY, Still contains ice  

E-Print Network [OSTI]

MEAT, POULTRY, SEAFOOD Still contains ice crystals and feels as cold, there will be some texture and Clavor loss. Discard DAIRY Still contains ice crystals and feels Ice cream, frozen yogurt Discard Discard Cheese (soft and semi-soft) Refreeze. May

Liskiewicz, Maciej

393

Hydrothermal Resources Fact Sheet  

Broader source: Energy.gov (indexed) [DOE]

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May Jun Jul(Summary) "ofEarly Career Scientists'Montana.ProgramJulietip sheetK-4In 2013DepartmentAgenda forThisEnergy

394

RMOTC - Library - Fact Sheets  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May JunDatastreamsmmcrcalgovInstrumentsrucLas ConchasPassive Solar HomePromising Science for1 20115, 2001Data sets Notice:Fact Sheets

395

ARM - Program Fact Sheets  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May JunDatastreamsmmcrcalgovInstrumentsruc Documentation RUC :ProductsSCM Forcing Data Derived from NWPMaterialsProgram Fact Sheets

396

ARM - Fact Sheets  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May JunDatastreamsmmcrcal Documentation(AVIRIS) ProductsAirborneOctober 11, 2011 [Facility News] Final Recovery ActJanuaryFact Sheets

397

WIPP - Fact Sheets  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May Jun Jul(Summary)morphinanInformation Desert SouthwestTechnologies | Blandine Jerome VelenciaNewsNews This pageRuralFact Sheets

398

SWPF Fact Sheet  

Office of Environmental Management (EM)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May Jun Jul(Summary) "of Energy Power Systems Engineering Research andReasonableLuncheon -- As|RichardMeetingSTEMFACT SHEET: SALT

399

ice | proceedings Forensic Engineering  

E-Print Network [OSTI]

ice | proceedings Forensic Engineering Volume 165 Issue FE4 November 2012 Forensic Engineering or economic damage. Research and practice papers are sought on traditional or modern forensic engineering, design and construction. Topics covered also include research and education best practice in forensic

Mottram, Toby

400

Metamaterial flexible sheets could transform optics  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Metamaterial flexible sheets could transform optics Metamaterial flexible sheets could transform optics Advances would boost security screening systems, infrared thermal cameras,...

Note: This page contains sample records for the topic "greenland ice sheet" 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.


401

Hail ice impact on composite structures at glancing angles  

E-Print Network [OSTI]

investigation of high velocity ice impacts on woven carbon/and ice sphere. .by trailing ice fragments. ..

Funai, Sho

2012-01-01T23:59:59.000Z

402

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

E-Print Network [OSTI]

temperature reconstruction from water isotopes in ice cores.temperature reconstruction from water isotopes in ice cores,Finkel, Changes in deep-water formation during the Younger

Kobashi, Takuro

2007-01-01T23:59:59.000Z

403

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

SciTech Connect (OSTI)

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

404

Contents Inquiry Sheet attached (Master Course: Blue sheet, Doctor Course: Light green sheet)  

E-Print Network [OSTI]

of energy and natural resources and the subsequent production of equally large amount of waste#12;#12; Contents Inquiry Sheet attached (Master Course: Blue sheet, Doctor Course: Light green and waste have lead to serious environmental contamination. The earth system be- comes increasingly

Yamamoto, Hirosuke

405

Contents Inquiry Sheet attached (Master Course: Blue sheet, Doctor Course: Light green sheet)  

E-Print Network [OSTI]

1 #12;#12; Contents Inquiry Sheet attached (Master Course: Blue sheet, Doctor Course: Light green countries, long-term economic growth results in the consumption of a vast amount of energy and natural resources and the subsequent production of equally large amount of waste. In developing countries

Yamamoto, Hirosuke

406

Coevolution of continental ice cover and permafrost extent over the last glacial-interglacial cycle in North  

E-Print Network [OSTI]

in North America Lev Tarasov1 and W. R. Peltier2 Received 14 August 2006; revised 20 March 2007; accepted both the most intense growth and recession phases. Citation: Tarasov, L., and W. R. Peltier (2007 of ice sheets across the North American continent [e.g., Tarasov and Peltier, 1999; Marshall et al., 2000

Peltier, W. Richard

407

Formation of high density amorphous ice by decompression of ice VII and ice VIII at 135 K  

E-Print Network [OSTI]

of ice Ih and are found to have very similar structures. By cooling liquid water along the water trans- forms into ice VIII when cooled . With this in mind Klug et al. were able to produce low densityFormation of high density amorphous ice by decompression of ice VII and ice VIII at 135 K Carl Mc

McBride, Carl

408

Hidden force floating ice  

E-Print Network [OSTI]

Because of the segmental specific-heat disparity of the hydrogen bond (O:H-O) and the Coulomb repulsion between oxygen ions, cooling elongates the O:H-O bond at freezing by stretching its containing angle and shortening the H-O bond with an association of larger O:H elongation, which makes ice less dense than water, allowing it to float.

Chang Q. Sun

2015-01-17T23:59:59.000Z

409

Ice Storm Supercomputer  

ScienceCinema (OSTI)

"A new Idaho National Laboratory supercomputer is helping scientists create more realistic simulations of nuclear fuel. Dubbed 'Ice Storm,' this 2048-processor machine allows researchers to model and predict the complex physics behind nuclear reactor behavior. And with a new visualization lab, the team can see the results of its simulations on the big screen." For more information about INL research, visit http://www.facebook.com/idahonationallaboratory.

None

2013-05-28T23:59:59.000Z

410

PRESS RELEASE I PARIS I 24 AOUT 2014 Tropical glaciers have responded to episodes of cooling in Greenland and the Antarctic  

E-Print Network [OSTI]

in Greenland and the Antarctic over the past 20,000 years, according to a study carried out mainly glaciers are found) show that these glaciers expanded not only during cooling over Greenland (12,000 years Reversal, or ACR), while temperatures in Greenland were relatively warm. In contrast, the following period

van Tiggelen, Bart

411

Correcting the MODIS snow albedo bias in Greenland based on in situ GC-Net measurements: Implications for the surface energy budget  

E-Print Network [OSTI]

Correcting the MODIS snow albedo bias in Greenland based on in situ GC-Net measurements). We have documented a systematic negative bias for SZA>55-60 in Greenland. This study uses in situ data from the Greenland Climate Network (GC-Net) to characterize and empirically correct the MODIS snow

Zender, Charles

412

The impact of Greenland on the predictability of European weather systems Supervisors: Sue Gray (U. Reading), Ian Renfrew (U. East Anglia) and Richard Swinbank (Met  

E-Print Network [OSTI]

The impact of Greenland on the predictability of European weather systems Supervisors: Sue Gray (U-to-high latitude of Greenland means it has a major influence on the atmospheric circulation of the North Atlantic by the presence of Greenland as is the atmosphere well downstream, for example over the British Isles

Renfrew, Ian

413

Microcomponent chemical process sheet architecture  

DOE Patents [OSTI]

The invention is a microcomponent sheet architecture wherein macroscale unit processes are performed by microscale components. The sheet architecture may be a single laminate with a plurality of separate microcomponent sections or the sheet architecture may be a plurality of laminates with one or more microcomponent sections on each laminate. Each microcomponent or plurality of like microcomponents perform at least one chemical process unit operation. A first laminate having a plurality of like first microcomponents is combined with at least a second laminate having a plurality of like second microcomponents thereby combining at least two unit operations to achieve a system operation. 26 figs.

Wegeng, R.S.; Drost, M.K.; Call, C.J.; Birmingham, J.G.; McDonald, C.E.; Kurath, D.E.; Friedrich, M.

1998-09-22T23:59:59.000Z

414

Microcomponent chemical process sheet architecture  

DOE Patents [OSTI]

The invention is a microcomponent sheet architecture wherein macroscale unit processes are performed by microscale components. The sheet architecture may be a single laminate with a plurality of separate microcomponent sections or the sheet architecture may be a plurality of laminates with one or more microcomponent sections on each laminate. Each microcomponent or plurality of like microcomponents perform at least one chemical process unit operation. A first laminate having a plurality of like first microcomponents is combined with at least a second laminate having a plurality of like second microcomponents thereby combining at least two unit operations to achieve a system operation.

Wegeng, Robert S. (Richland, WA); Drost, M. Kevin (Richland, WA); Call, Charles J. (Pasco, WA); Birmingham, Joseph G. (Richland, WA); McDonald, Carolyn Evans (Richland, WA); Kurath, Dean E. (Benton County, WA); Friedrich, Michele (Prosser, WA)

1998-01-01T23:59:59.000Z

415

Engineering Notes Ice Shape Characterization Using  

E-Print Network [OSTI]

Engineering Notes Ice Shape Characterization Using Self-Organizing Maps Stephen T. McClain Baylor. Introduction DURING the validation and verification of ice accretion codes, predicted ice shapes must be compared with experimental measurements of wind-tunnel or atmospheric ice shapes. Current methods for ice

Tino, Peter

416

Biomass Surface Characterization Laboratory (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet provides information about Biomass Surface Characterization Laboratory capabilities and applications at NREL.

Not Available

2012-04-01T23:59:59.000Z

417

Biochemical Conversion Pilot Plant (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet provides information about Biochemical Conversion Pilot Plant capabilities and resources at NREL.

Not Available

2012-06-01T23:59:59.000Z

418

Ice Mass Balance Buoy: An Instrument to Measure and Attribute Changes in Ice Thickness  

E-Print Network [OSTI]

Ice Mass Balance Buoy: An Instrument to Measure and Attribute Changes in Ice Thickness Jacqueline A the Ice Mass Balance buoy (IMB) in response to the need for monitoring changes in the thickness of the Arctic sea ice cover. The IMB is an autonomous, ice-based system. IMB buoys provide a time series of ice

Geiger, Cathleen

419

Pollution Transport From North America to Greenland During Summer 2008  

SciTech Connect (OSTI)

Ozone pollution transported to the Arctic is a significant concern because of the rapid, enhanced warming in high northern latitudes, which is caused, in part, by short lived climate forcers, such as ozone. Long range transport of pollution contributes to background and episodic ozone levels in the Arctic. However, the extent to which plumes are photochemically active during transport, particularly during the summer, is uncertain. Regional chemical transport model simulations are used to examine photochemical production of ozone in air masses originating from boreal fire and anthropogenic emissions over North America and during their transport toward the Arctic during early July 2008. Model results shows good agreement with aircraft data collected over boreal fire source regions in Canada and several days downwind over Greenland during the study period. Pollutant plumes were transported east and north towards the Arctic and show significant ozone enhancements downwind of source regions. Anthropogenic plumes were more photochemically active than fire plumes. Together, both sources made an important contribution to ozone in pollution plumes transported to the Arctic.

Thomas, J. L.; Raut, Jean-Christophe; Law, K. S.; Marelle, L.; Ancellet, G.; Ravetta, F.; Fast, Jerome D.; Pfister, G.; Emmons, L.; Diskin, G. S.; Weinheimer, Andrew J.; Roiger, A.; Schlager, H.

2013-04-10T23:59:59.000Z

420

Pollution transport from North America to Greenland during summer 2008  

SciTech Connect (OSTI)

Ozone pollution transported to the Arctic is a significant concern because of the rapid, enhanced warming in high northern latitudes, which is caused, in part, by short lived climate forcers, such as ozone. Long range transport of pollution contributes to background and episodic ozone levels in the Arctic. However, the extent to which plumes are photochemically active during transport, particularly during the summer, is uncertain. Regional chemical transport model simulations are used to examine photochemical production 8 of ozone in air masses originating from boreal fire and anthropogenic emissions over North America and during their transport toward the Arctic during early July 2008. Model results shows good agreement with aircraft data collected over boreal fire source regions in Canada and several days down-wind over Greenland during the study period. Pollutant plumes were transported east and north towards the Arctic and show significant ozone enhancements downwind of source regions. Anthropogenic plumes were more photochemically active than fire plumes. Together, both sources made an important contribution to ozone in pollution plumes transported to the Arctic.

Thomas, J. L.; Raut, Jean-Christophe; Law, K. S.; Marelle, L.; Ancellet, G.; Ravetta, F.; Fast, Jerome D.; Pfister, G.; Emmons, L.; Diskin, G. S.; Weinheimer, Andrew J.; Roiger, A.; Schlager, H.

2013-04-10T23:59:59.000Z

Note: This page contains sample records for the topic "greenland ice sheet" 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.


421

Large Sheet Process Consolidation Project  

E-Print Network [OSTI]

The purpose of this project is to reduce labor costs through the consolidation of large sheet processes into the Beta and Alpha manufacturing plants. The consolidation of equipment and departments will allow for the reduction of indirect labor...

Johnson, Keith

2005-12-16T23:59:59.000Z

422

Decommissioning Under CERCLA Information Sheet  

Broader source: Energy.gov [DOE]

This Question and Answer (Q&A) Sheet discusses the use of removal authority in the conduct of decommissioning activities, consistent with the Policy on Decommissioning of Department of Energy...

423

Measurements and Characterization (Fact Sheet)  

SciTech Connect (OSTI)

Capabilities fact sheet for the National Center for Photovoltaics: Measurements and Characterization that includes scope, core competencies and capabilities, and contact/web information for Analytical Microscopy, Electro-Optical Characterization, Surface Analysis, and Cell and Module Performance.

Not Available

2011-06-01T23:59:59.000Z

424

Concentrating Solar Power (Fact Sheet)  

SciTech Connect (OSTI)

Fact sheet describing the overall capabilities of the NREL CSP Program: collector/receiver characterization, advanced reflector and absorber materials, thermal storage and advanced heat transfer fluids, and CSP modeling and analysis.

Not Available

2010-08-01T23:59:59.000Z

425

2, 383397, 2008 Extreme surface melt  

E-Print Network [OSTI]

surface snowmelt over high elevations (above 2000 m) of the Greenland ice sheet during summer of 2007Pa atmospheric thick- ness, and the net surface energy flux, linked in turn to southerly airflow over the ice10 Scanning Multichannel Microwave Radiometer (SMMR, 1979­1987) and the Special Sensor Microwave/Imager (SSM

Paris-Sud XI, Université de

426

Fire and Ice Issue 9  

E-Print Network [OSTI]

s FIRE AND ICE # 9 IB FIRE ICE #9 A Blake/Avon slash fanzine r Available from: Kathleen Resch POBox 1766 Temple City, CA 91780 Kathleener@aol.com FIRE AND ICE # 9copyright May, 2005 by Kathleen Resch for the contributors. No reprints... or reproduction without the written permission ofthe author/artist This is an amateur publication and is not p intended to infringe upon the rights ofany holders of"Blake's 7" copyrights. FIRE AND ICE 9 TABLE OF CONTENTS LEAVING ROOM 101 by Nova 2 TOO MANY...

Multiple Contributors

2005-01-01T23:59:59.000Z

427

Energy information sheets, September 1996  

SciTech Connect (OSTI)

The National Energy Information Center (NEIC), as part of its mission, provides energy information and referral assistance to Federal, State, and local governments, the academic community, business and industrial organizations, and the public. The Energy Information Sheets was developed to provide general information on various aspects of fuel production, prices, consumption, and capability. Additional information on related subject matter can be found in other Energy Information Administration (EIA) publications as referenced at the end of each sheet.

NONE

1996-09-01T23:59:59.000Z

428

Energy information sheets, July 1998  

SciTech Connect (OSTI)

The National Energy Information Center (NEIC), as part of its mission, provides energy information and referral assistance to Federal, State, and local governments, the academic community, business and industrial organizations, and the public. The Energy Information Sheets was developed to provide general information on various aspects of fuel production, prices, consumption, and capability. Additional information on related subject matter can be found in other Energy Information Administration (EIA) publications as referenced at the end of each sheet.

NONE

1998-07-01T23:59:59.000Z

429

Horizontal electromagnetic casting of thin metal sheets  

DOE Patents [OSTI]

Thin metal sheets are cast by magnetically suspending molten metal deposited within a ferromagnetic yoke and between AC conducting coils and linearly displacing the magnetically levitated liquid metal while it is being cooled to form a solid metal sheet. Magnetic flux increases as the molten metal sheet moves downward and decreases as the molten metal sheet moves upward to stabilize the sheet and maintain it in equilibrium as it is linearly displaced and solidified by cooling gases. A conducting shield is electrically coupled to the molten metal sheet by means of either metal sheet engaging rollers or brushes on the solidified metal, and by means of an electrode in the vessel containing the molten metal thereby providing a return path for the eddy currents induced in the metal sheet by the AC coil generated magnetic flux. Variation in the geometry of the conducting shield allows the magnetic flux between the metal sheet and the conducting shield to be varied and the thickness in surface quality of the metal sheet to be controlled. Side guards provide lateral containment for the molten metal sheet and stabilize and shape the magnetic field while a leader sheet having electromagnetic characteristics similar to those of the metal sheet is used to start the casting process and precedes the molten metal sheet through the magnet and forms a continuous sheet therewith. The magnet may be either U-shaped with a single racetrack coil or may be rectangular with a pair of facing bedstead coils.

Hull, John R. (Hinsdale, IL); Lari, Robert J. (Aurora, IL); Praeg, Walter F. (Palos Park, IL); Turner, Larry R. (Naperville, IL)

1987-01-01T23:59:59.000Z

430

Horizontal electromagnetic casting of thin metal sheets  

DOE Patents [OSTI]

Thin metal sheets are cast by magnetically suspending molten metal deposited within a ferromagnetic yoke and between AC conducting coils and linearly displacing the magnetically levitated liquid metal while it is being cooled to form a solid metal sheet. Magnetic flux increases as the molten metal sheet moves downward and decreases as the molten metal sheet moves upward to stabilize the sheet and maintain it in equilibrium as it is linearly displaced and solidified by cooling gases. A conducting shield is electrically coupled to the molten metal sheet by means of either metal sheet engaging rollers or brushes on the solidified metal, and by means of an electrode in the vessel containing the molten metal thereby providing a return path for the eddy currents induced in the metal sheet by the AC coil generated magnetic flux. Variation in the geometry of the conducting shield allows the magnetic flux between the metal sheet and the conducting shield to be varied and the thickness in surface quality of the metal sheet to be controlled. Side guards provide lateral containment for the molten metal sheet and stabilize and shape the magnetic field while a leader sheet having electromagnetic characteristics similar to those of the metal sheet is used to start the casting process and precedes the molten metal sheet through the magnet and forms a continuous sheet therewith. The magnet may be either U-shaped with a single racetrack coil or may be rectangular with a pair of facing bedstead coils.

Hull, John R. (Hinsdale, IL); Lari, Robert J. (Aurora, IL); Praeg, Walter F. (Palos Park, IL); Turner, Larry R. (Naperville, IL)

1988-01-01T23:59:59.000Z

431

ICE Raids: Compounding Production, Contradiction, and Capitalism  

E-Print Network [OSTI]

is just a cheap way of boosting ICE criminal alien arrestRegardless of whether or not ICE is motivated by maintainingWorkers in America: Factories and ICE Raids Produce Citizens

Reas, Elizabeth I

2009-01-01T23:59:59.000Z

432

ICE Pulse Oximeter Smart Alarm App Requirements  

E-Print Network [OSTI]

ICE Pulse Oximeter Smart Alarm App Requirements 6 March 2012 Revision 0 for an Integrated Clinical Environment (ICE) pulse oximetry monitoring app that provides.2 References [Purpose: List all ICE standards, and other standards and references

Huth, Michael

433

Biogeochemistry in Sea Ice: CICE model developments  

SciTech Connect (OSTI)

Polar primary production unfolds in a dynamic sea ice environment, and the interactions of sea ice with ocean support and mediate this production. In spring, for example, fresh melt water contributes to the shoaling of the mixed layer enhancing ice edge blooms. In contrast, sea ice formation in the fall reduces light penetration to the upper ocean slowing primary production in marine waters. Polar biogeochemical modeling studies typically consider these types of ice-ocean interactions. However, sea ice itself is a biogeochemically active medium, contributing a significant and, possibly, essential source of primary production to polar regions in early spring and fall. Here we present numerical simulations using the Los Alamos Sea Ice Model (CICE) with prognostic salinity and sea ice biogeochemistry. This study investigates the relationship between sea ice multiphase physics and sea ice productivity. Of particular emphasis are the processes of gravity drainage, melt water flushing, and snow loading. During sea ice formation, desalination by gravity drainage facilitates nutrient exchange between ocean and ice maintaining ice algal blooms in early spring. Melt water flushing releases ice algae and nutrients to underlying waters limiting ice production. Finally, snow loading, particularly in the Southern Ocean, forces sea ice below the ocean surface driving an upward flow of nutrient rich water into the ice to the benefit of interior and freeboard communities. Incorporating ice microphysics in CICE has given us an important tool for assessing the importance of these processes for polar algal production at global scales.

Jeffery, Nicole [Los Alamos National Laboratory; Hunke, Elizabeth [Los Alamos National Laboratory; Elliott, Scott [Los Alamos National Laboratory; Turner, Adrian [Los Alamos National Laboratory

2012-06-18T23:59:59.000Z

434

Therapeutic Hypothermia: Protective Cooling Using Medical Ice...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Therapeutic Hypothermia: Protective Cooling Using Medical Ice Slurry Technology available for licensing: Proprietary method and equipment for making an ice slurry coolant to induce...

435

Save Energy Now - South Carolina Project Fact Sheet | Department...  

Broader source: Energy.gov (indexed) [DOE]

- South Carolina Project Fact Sheet Save Energy Now - South Carolina Project Fact Sheet This fact sheet contains details regarding a Save Energy Now industrial energy efficiency...

436

Fire and Ice Issue 2  

E-Print Network [OSTI]

^ $$% i&l /P^ \\0 rffej FIRE AND ICE AVAILABLE FROM Kathleen Resch PO Box 1766 Temple City, CA 91780 FIRE AND ICE II TABLE OF CONTENTS COVER by Phoenix FRONTISPIECE by Gayle Feyrer "Flashpoint" by Rachel Duncan 1 PEDESTAL by Thomas 2 "A Damn Fine...

Multiple Contributors

1993-01-01T23:59:59.000Z

437

Improved Reliability of PV Modules with Lexan PC Sheet-Front...  

Broader source: Energy.gov (indexed) [DOE]

IMPROVED RELIABILITY OF PV MODULES WITH LEXAN(tm) (PC ) SHEET - FRONT SHEET NORYL(tm) (PPE) SHEET - BACK SHEET NORYL(tm) Sheet for back sheet application LEXAN(tm) sheet for front...

438

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

439

Dynamics of ice shelf rift propagation and iceberg calving inferred from geodetic and seismic observations  

E-Print Network [OSTI]

2. Ice Shelves . . . . . . . . . . . . . . . . .5. Ice Rheology . . . . . . . . . . . . . 6.vi Calving Glaciers and Ice

Bassis, Jeremy N.

2007-01-01T23:59:59.000Z

440

Examinations of ice formation processes in Florida cumuli using ice nuclei measurements of anvil ice crystal particle residues  

E-Print Network [OSTI]

importance of different ice formation processes in cumuli and the cirrus anvils they produce. Cirrus playExaminations of ice formation processes in Florida cumuli using ice nuclei measurements of anvil ice crystal particle residues Anthony J. Prenni,1 Paul J. DeMott,1 Cynthia Twohy,2 Michael R. Poellot

Note: This page contains sample records for the topic "greenland ice sheet" 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.


441

Modeling the response of subglacial drainage at Paakitsoq, West Greenland, to 21st century climate change  

E-Print Network [OSTI]

, and into the future. Here, we apply a physically-based, subglacial hydrological model to the Paakitsoq region, west Greenland, and run it into the future to calculate patterns of daily subglacial water pressure fluctuations in response to climatic warming. The model...

Mayaud, Jerome R.; Banwell, Alison F.; Arnold, Neil S.; Willis, Ian C.

2015-01-22T23:59:59.000Z

442

Glass Concrete Thin Sheets Reinforced with Prestressed Aramid Fabrics  

E-Print Network [OSTI]

Glass Concrete Thin Sheets Reinforced with Prestressed Aramid Fabrics Gregor Vilkner Submitted Glass Concrete Thin Sheets Reinforced with Prestressed Aramid Fabrics Gregor Vilkner Thin sheet concrete presented in this work explored the possibilities of prestressing thin sheet glass concrete products

Meyer, Christian

443

Ice deformation near SHEBA R. W. Lindsay  

E-Print Network [OSTI]

in the vicinity of the Surface Heat Budget of the Arctic Ocean (SHEBA) ice camp that is suitable for forcing factor for regional heat fluxes, ice growth and melt rates, and ice strength [Maykut, 1982Ice deformation near SHEBA R. W. Lindsay Polar Science Center, University of Washington, Seattle

Lindsay, Ron

444

4, 709732, 2007 Ice-shelf ocean  

E-Print Network [OSTI]

OSD 4, 709732, 2007 Ice-shelf ocean interactions at Fimbul Ice Shelf M. R. Price Title Page published in Ocean Science Discussions are under open-access review for the journal Ocean Science Ice-shelf ocean interactions at Fimbul Ice Shelf, Antarctica from oxygen isotope ratio measurements M. R. Price 1

Boyer, Edmond

445

Climate Change and Variability Lake Ice, Fishes  

E-Print Network [OSTI]

#12;Climate Change and Variability Lake Ice, Fishes and Water Levels John J. Magnuson Center to everything else." #12;The Invisible Present The Invisible Place Magnuson 2006 #12;Ice-on Day 2007 Peter W. Schmitz Photo Local Lake Mendota #12;Ice Breakup 2010 Lake Mendota March 20 #12;March 21 Ice Breakup 2010

Sheridan, Jennifer

446

Photovoltaic Reliability and Engineering (Revised) (Fact Sheet)  

SciTech Connect (OSTI)

Capabilities fact sheet for the National Center for Photovoltaics: Photovoltaic Reliability and Engineering. One-sided sheet that includes Scope, Core Competencies and Capabilities, and Contact/Web information.

Not Available

2011-06-01T23:59:59.000Z

447

2011-12 PROSPECTUS2011-12 PROSPECTUS WESLEYAN MEN'S ICE HOCKEYWESLEYAN MEN'S ICE HOCKEY  

E-Print Network [OSTI]

- ponents in its inaugural season. Former bench boss Dave Snyder, in whose honor the Wesleyan ice rink2011-12 PROSPECTUS2011-12 PROSPECTUS WESLEYAN MEN'S ICE HOCKEYWESLEYAN MEN'S ICE HOCKEY #12....................................Chris Potter/Jeff Gilarde Men's Ice Hockey..............Chris Potter Women's Ice Hockey.........Jodi Mc

Devoto, Stephen H.

448

Impact of underwater-ice evolution on Arctic summer sea ice  

E-Print Network [OSTI]

Impact of underwater-ice evolution on Arctic summer sea ice Dirk Notz,1,4 Miles G. McPhee,2 M. Grae the simultaneous growth and ablation of a layer of ice between an under-ice melt pond and the underlying ocean. Such ``false bottoms'' are the only significant source of ice formation in the Arctic during summer. Analytical

Worster, M. Grae

449

Ice Shelf Water plume flow beneath Filchner-Ronne Ice Shelf, Antarctica  

E-Print Network [OSTI]

Ice Shelf Water plume flow beneath Filchner-Ronne Ice Shelf, Antarctica Paul R. Holland,1 Daniel L Filchner- Ronne Ice Shelf, Antarctica and its underlying ocean cavity. Ice Shelf Water (ISW) plumes are initiated by the freshwater released from a melting ice shelf and, if they rise, may become supercooled

Feltham, Daniel

450

ORIGINAL PAPER A bacterial ice-binding protein from the Vostok ice core  

E-Print Network [OSTI]

to produce a 54 kDa ice-binding protein (GenBank EU694412) that is similar to ice-binding proteins previously- vival at sub-zero temperatures by producing proteins that bind to and inhibit the growth of ice crystalsORIGINAL PAPER A bacterial ice-binding protein from the Vostok ice core James A. Raymond ? Brent C

Christner, Brent C.

451

The Effects of Rotation and Ice Shelf Topography on Frazil-Laden Ice Shelf Water Plumes  

E-Print Network [OSTI]

, Antarctica. In addition, it is found that the model only produces reasonable marine ice formation rates whenThe Effects of Rotation and Ice Shelf Topography on Frazil-Laden Ice Shelf Water Plumes PAUL R of the dynamics and thermodynamics of a plume of meltwater at the base of an ice shelf is presented. Such ice

Feltham, Daniel

452

Global simulations of ice nucleation and ice supersaturation with an improved cloud scheme in the Community  

E-Print Network [OSTI]

and supersaturation in CAM. The new model is able to reproduce field observations of ice mass and mixed phase cloud are sensitive to the parameterization of ice clouds. These results indicate that ice clouds are potentiallyGlobal simulations of ice nucleation and ice supersaturation with an improved cloud scheme

Gettelman, Andrew

453

Sea-ice thickness measurement based on the dispersion of ice swell  

E-Print Network [OSTI]

-azimuth angles. The parameterization, that includes finding the best modeled ice thickness, is performed by usingSea-ice thickness measurement based on the dispersion of ice swell David Marsana) ISTerre, CNRS propagating in the Arctic sea ice cover is exploited in order to locally measure the ice thickness

454

Electrical properties of saline ices and ice-silicate mixtures: geophysical and astrobiological consequences (Invited)  

E-Print Network [OSTI]

MR22A-05 Electrical properties of saline ices and ice-silicate mixtures: geophysical) electrical-properties measurements of laboratory- produced saline ice, salt hydrates, and ice-silicate cutoff. In ice-silicate mixtures, brine channels are evident above the eutectic temperature only when

Stillman, David E.

455

Comment on ``A quantitative framework for interpretation of basal ice facies formed by ice  

E-Print Network [OSTI]

heave would be expected to produce were revealed beneath the Kamb Ice Stream by the pioneering boreholeComment on ``A quantitative framework for interpretation of basal ice facies formed by ice quantitative framework for interpretation of basal ice facies formed by ice accretion over subglacial sediment

Worster, M. Grae

456

Federal Incentives for Water Power (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet describes the federal incentives available as of April 2013 for the development of water power technologies.

Not Available

2013-05-01T23:59:59.000Z

457

Biomass Compositional Analysis Laboratory (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet provides information about Biomass Compositional Analysis Laboratory (BCAL) capabilities and applications at NREL's National Bioenergy Center.

Not Available

2011-07-01T23:59:59.000Z

458

Fuel Synthesis Catalysis Laboratory (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet provides information about Fuel Synthesis Catalysis Laboratory capabilities and applications at NREL's National Bioenergy Center.

Not Available

2011-07-01T23:59:59.000Z

459

Fact Sheet: Energy Storage Technology Advancement Partnership...  

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

Technology Advancement Partnership (October 2012) Fact Sheet: Energy Storage Technology Advancement Partnership (October 2012) The Energy Storage Technology Advancement Partnership...

460

Home Energy Score Data Collection Sheet  

Broader source: Energy.gov [DOE]

Input sheet for qualified assessors to collect data for input into the Home Energy Scoring Tool for evaluation.

Note: This page contains sample records for the topic "greenland ice sheet" 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.


461

Fuel Synthesis Catalysis Laboratory (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet provides information about Fuel Synthesis Catalysis Laboratory capabilities and applications at NREL's National Bioenergy Center.

Not Available

2013-07-01T23:59:59.000Z

462

Telling the NREL Story (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet explains NREL's efforts to inform staff on consistent messaging and resources for communicating to laboratory stakeholders.

Not Available

2014-07-01T23:59:59.000Z

463

Utility Rebates and Incentive Programs (Fact Sheet)  

SciTech Connect (OSTI)

Fact sheet overview of the Federal Utility Partnership Working Group (FUPWG), including group objectives, activities, and services.

Not Available

2009-07-01T23:59:59.000Z

464

Algal Biofuels Research Laboratory (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet provides information about Algal Biofuels Research Laboratory capabilities and applications at NREL's National Bioenergy Center.

Not Available

2011-08-01T23:59:59.000Z

465

Manifold free multiple sheet superplastic forming  

DOE Patents [OSTI]

Fluid-forming compositions in a container attached to enclosed adjacent sheets are heated to relatively high temperatures to generate fluids (gases) that effect inflation of the sheets. Fluid rates to the enclosed space between the sheets can be regulated by the canal from the container. Inflated articles can be produced by a continuous, rather than batch-type, process.

Elmer, John W. (Danville, CA); Bridges, Robert L. (Knoxville, TN)

2001-01-01T23:59:59.000Z

466

Manifold free multiple sheet superplastic forming  

DOE Patents [OSTI]

Fluid-forming compositions in a container attached to enclosed adjacent sheets are heated to relatively high temperatures to generate fluids (gases) that effect inflation of the sheets. Fluid rates to the enclosed space between the sheets can be regulated by the canal from the container. Inflated articles can be produced by a continuous, rather than batch-type, process.

Elmer, John W.; Bridges, Robert L.

2004-01-13T23:59:59.000Z

467

Project Fact Sheet Project Update  

E-Print Network [OSTI]

Project Fact Sheet Project Update: Project Brief: A state of the art facility, at Hammersmith information visit the Faculty of Medicine web pages http://www1.imperial.ac.uk/medicine/ Construction Project Team: Project Facts & Figures: Budget: £60 000 000 Funding Source: SRIF II (Imperial College), GSK, MRC

468

Project Fact Sheet Project Update  

E-Print Network [OSTI]

Project Fact Sheet Project Update: Project Brief: The refurbishment of the instrumentation equipment. This project encompasses refurbishment work on over 1,150m2 of laboratory space across four, the completed project will allow researchers to expand their work in satellite instrumentation, the fabrication

469

Project Fact Sheet Project Brief  

E-Print Network [OSTI]

Project Fact Sheet Project Brief: In the first phase of the Union Building re.union.ic.ac.uk/marketing/building Construction Project Team: Project Facts & Figures: Budget: £1,400,000 Funding Source: Capital Plan and Imperial College Union reserves Construction Project Programme: Start on Site: August 2006 End Date: March

470

Project Fact Sheet Project Brief  

E-Print Network [OSTI]

Project Fact Sheet Project Brief: Construction Project Team: Project Facts & Figures: Budget: £500,000 Funding Source: Capital Construction Project Programme: Start on Site: October 2010 End Date : April 2011 Occupation Date: n/a For further information contact Project Manager as listed above or the Imperial College

471

Project Fact Sheet Project Brief  

E-Print Network [OSTI]

Project Fact Sheet Project Brief: This project refurbished half of the 5th and 7th floors on the Faculty of Medicine, please visit: http://www1.imperial.ac.uk/medicine/ Construction Project Team: Project Facts & Figures: Budget: £3,500,000 Funding Source: SRIF III Construction Project Programme: Start

472

Finance Degree Curriculum Information Sheet  

E-Print Network [OSTI]

Finance Degree Curriculum Information Sheet Business Core 33:010:275-Intro. to Managerial:390:310-Financial Management for Finance Majors (3)* 33:620:301-Intro to Management (3)** 33:620:302-Management Management (3) Required Finance Courses 33:390:380-Investment Analysis (3) (pre-req: 33:390:310) 33

Lin, Xiaodong

473

Finance Degree Curriculum Information Sheet  

E-Print Network [OSTI]

Finance Degree Curriculum Information Sheet 33:010:275-Intro. to Managerial Accounting (3) (pre-req: 33:010:272) 33:011:300-Business Forum (2) 33:390:310-Financial Management for Finance Majors (3)* 33:390:400-Corporate Finance (3) (pre-req: 33:390:310) 4 Finance electives (12) * Beginning Fall 2013

Lin, Xiaodong

474

Strategic Energy Analysis (Fact Sheet)  

SciTech Connect (OSTI)

NREL complements its scientific research with high-quality, credible, technology-neutral, objective analysis that informs policy and investment decisions as renewable energy and energy efficiency technologies move from innovation through integration. This sheet highlights NREL's analytical capabilities and achievements.

Not Available

2014-02-01T23:59:59.000Z

475

Product Sheet Wall Mount Lift  

E-Print Network [OSTI]

Product Sheet Wall Mount Lift Ergotron Neo-FlexTM 870-05-061, rev. 12/11/07 www. Less effort. Feel the difference. Add greater range of movement to your LCD display or TV with the Neo-Flex Wall Mount Lift! CF patented lift-and-pivot motion technology adjusts with a light touch. Raise

Saskatchewan, University of

476

Magnetic Resonance Facility (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet provides information about Magnetic Resonance Facility capabilities and applications at NREL's National Bioenergy Center. Liquid and solid-state analysis capability for a variety of biomass, photovoltaic, and materials characterization applications across NREL. NREL scientists analyze solid and liquid samples on three nuclear magnetic resonance (NMR) spectrometers as well as an electron paramagnetic resonance (EPR) spectrometer.

Not Available

2012-03-01T23:59:59.000Z

477

Technology Performance Exchange (Fact Sheet)  

SciTech Connect (OSTI)

This fact sheet, 'The Technology Performance Exchange' will be presented at the ET Summit, held at the Pasadena Convention Center on October 15-17, 2012. The Technology Performance Exchange will be a centralized, Web-based portal for finding and sharing energy performance data for commercial building technologies.

Not Available

2012-10-01T23:59:59.000Z

478

Project Fact Sheet Project Update  

E-Print Network [OSTI]

Project Fact Sheet Project Update: Project Brief: The works cover the refurbishment of floors 4, 5, with `wet' labs for molecular biology, materials characterisation, cell culture and flow studies, and `dry operating theatre. The Bionanotechnology Centre is one of the projects funded from the UK Government's £20

479

Method of forming clathrate ice  

DOE Patents [OSTI]

A method of forming clathrate ice in a supercooled water-based liquid contained in a vessel is disclosed. Initially, an oscillator device is located in the liquid in the vessel. The oscillator device is then oscillated ultrasonically so that small crystals are formed in the liquid. These small crystals serve as seed crystals for ice formation in the liquid and thereby prevent supercooling of the liquid. Preferably, the oscillating device is controlled by a thermostat which initiates operation of the oscillator device when the temperature of the liquid is lowered to the freezing point. Thereafter, the operation of the oscillator device is terminated when ice is sensed in the liquid by an ice sensor.

Hino, Toshiyuki (Tokyo, JP); Gorski, Anthony J. (Lemont, IL)

1987-01-01T23:59:59.000Z

480

Method of forming calthrate ice  

DOE Patents [OSTI]

A method of forming clathrate ice in a supercooled water-based liquid contained in a vessel is disclosed. Initially, an oscillator device is located in the liquid in the vessel. The oscillator device is then oscillated ultransonically so that small crystals are formed in the liquid. Thes small crystals serve as seed crystals for ice formation in the liquid and thereby prevent supercooling of the liquid. Preferably, the oscillating device is controlled by a thermostat which initiates operation of the oscillator device when the temperature of the liquid is lowered to the freezing point. Thereafter, the operation of the oscillator device is terminated when ice is sensed in the liquid by an ice sensor.

Hino, T.; Gorski, A.J.

1985-09-30T23:59:59.000Z

Note: This page contains sample records for the topic "greenland ice sheet" 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.


481

Final Report for DOE grant DE-FG02-07ER64432 "New Grid and Discretization Technologies for Ocean and Ice Simulations"  

SciTech Connect (OSTI)

The work reported is in pursuit of these goals: high-quality unstructured, non-uniform Voronoi and Delaunay grids; improved finite element and finite volume discretization schemes; and improved finite element and finite volume discretization schemes. These are sought for application to spherical and three-dimensional applications suitable for ocean, atmosphere, ice-sheet, and other climate modeling applications.

Gunzburger, Max

2013-03-12T23:59:59.000Z

482

Step-wise changes in glacier flow speed coincide with calving and glacial earthquakes at Helheim Glacier, Greenland  

E-Print Network [OSTI]

[1] Geodetic observations show several large, sudden increases in flow speed at Helheim Glacier, one of Greenland's largest outlet glaciers, during summer, 2007. These step-like accelerations, detected along the length of the glacier, coincide...

Nettles, M.; Larsen, T.B.; Elosegui, P.; Hamilton, Gordon S.; Stearns, Leigh; Ahlstrom, A.P.; Davis, J.L.; Anderson, M.L.; de Juan, J.; Khan, S.A.; Stenseng, L.; Ekstrom, G.; Forsberg, R.

2008-12-30T23:59:59.000Z

483

An experimental and theoretical study of the ice accretion process during artificial and natural icing conditions  

E-Print Network [OSTI]

Real-time measurements of ice growth during artificial and natural icing conditions were conducted using an ultrasonic pulse-echo technique. This technique allows ice thickness to be measured with an accuracy of ?0.5 mm; ...

Kirby, Mark Samuel

1986-01-01T23:59:59.000Z

484

amorphous ice transition: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

artificial and natural icing conditions MIT - DSpace Summary: Real-time measurements of ice growth during artificial and natural icing conditions were conducted using an...

485

alpine deep ice: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

artificial and natural icing conditions MIT - DSpace Summary: Real-time measurements of ice growth during artificial and natural icing conditions were conducted using an...

486

An update on modeling land-ice/ocean interactions in CESM  

SciTech Connect (OSTI)

This talk is an update on ongoing land-ice/ocean coupling work within the Community Earth System Model (CESM). The coupling method is designed to allow simulation of a fully dynamic ice/ocean interface, while requiring minimal modification to the existing ocean model (the Parallel Ocean Program, POP). The method makes use of an immersed boundary method (IBM) to represent the geometry of the ice-ocean interface without requiring that the computational grid be modified in time. We show many of the remaining development challenges that need to be addressed in order to perform global, century long climate runs with fully coupled ocean and ice sheet models. These challenges include moving to a new grid where the computational pole is no longer at the true south pole and several changes to the coupler (the software tool used to communicate between model components) to allow the boundary between land and ocean to vary in time. We discuss benefits for ice/ocean coupling that would be gained from longer-term ocean model development to allow for natural salt fluxes (which conserve both water and salt mass, rather than water volume).

Asay-davis, Xylar [Los Alamos National Laboratory

2011-01-24T23:59:59.000Z

487

Improved Reliability of PV Modules with Lexan PC Sheet-Front...  

Broader source: Energy.gov (indexed) [DOE]

Improved Reliability of PV Modules with Lexan PC Sheet-Front Sheet, Noryl PPE Sheet-Back Sheet Improved Reliability of PV Modules with Lexan PC Sheet-Front Sheet, Noryl PPE...

488

Vapor deposition of water on graphitic surfaces: Formation of amorphous ice, bilayer ice, ice I, and liquid water  

SciTech Connect (OSTI)

Carbonaceous surfaces are a major source of atmospheric particles and could play an important role in the formation of ice. Here we investigate through molecular simulations the stability, metastability, and molecular pathways of deposition of amorphous ice, bilayer ice, and ice I from water vapor on graphitic and atomless Lennard-Jones surfaces as a function of temperature. We find that bilayer ice is the most stable ice polymorph for small cluster sizes, nevertheless it can grow metastable well above its region of thermodynamic stability. In agreement with experiments, the simulations predict that on increasing temperature the outcome of water deposition is amorphous ice, bilayer ice, ice I, and liquid water. The deposition nucleation of bilayer ice and ice I is preceded by the formation of small liquid clusters, which have two wetting states: bilayer pancake-like (wetting) at small cluster size and droplet-like (non-wetting) at larger cluster size. The wetting state of liquid clusters determines which ice polymorph is nucleated: bilayer ice nucleates from wetting bilayer liquid clusters and ice I from non-wetting liquid clusters. The maximum temperature for nucleation of bilayer ice on flat surfaces, T{sub B}{sup max} is given by the maximum temperature for which liquid water clusters reach the equilibrium melting line of bilayer ice as wetting bilayer clusters. Increasing water-surface attraction stabilizes the pancake-like wetting state of liquid clusters leading to larger T{sub B}{sup max} for the flat non-hydrogen bonding surfaces of this study. The findings of this study should be of relevance for the understanding of ice formation by deposition mode on carbonaceous atmospheric particles, including soot.

Lupi, Laura; Kastelowitz, Noah; Molinero, Valeria, E-mail: Valeria.Molinero@utah.edu [Department of Chemistry, The University of Utah, 315 South 1400 East, Salt Lake City, Utah 84112-0850 (United States)

2014-11-14T23:59:59.000Z

489

Ross Ice Shelf in situ radio-frequency ice attenuation  

E-Print Network [OSTI]

We have measured the in situ average electric field attenuation length for radio-frequency signals broadcast vertically through the Ross Ice Shelf. We chose a location, Moore Embayment, south of Minna Bluff, known for its high reflectivity at the ice-sea interface. We confirmed specular reflection and used the return pulses to measure the average attenuation length from 75-1250 MHz over the round-trip distance of 1155 m. We find the average electric field attenuation length to vary from 500 m at 75 MHz to 300 m at 1250 MHz, with an experimental uncertainty of 55 to 15 m. We discuss the implications for neutrino telescopes that use the radio technique and include the Ross Ice Shelf as part of their sensitive volume.

Taylor Barrella; Steven Barwick; David Saltzberg

2012-05-01T23:59:59.000Z

490

Miocene to recent ice elevation variations from the interior of the West Antarctic ice sheet: Constraints from geologic observations, cosmogenic  

E-Print Network [OSTI]

,n , Robert P. Ackert Jr.a , Allen E. Pope a,b , David Pollard c , Robert M. DeConto d a Department of Earth, University of Cambridge, Lensfield Road, CB2 1ER, England c Earth and Environmental Systems Institute-term observational constraints are however, rare. Here we present the first constraints on long-term (Miocene

Mukhopadhyay, Sujoy

491

Physical Controls on Ice Variability in the Bering Sea /  

E-Print Network [OSTI]

region. The model also produces less ice near much of thewinds (Figure 3.13c,d) produce more ice growth and more iceThe model produces variations in total ice area anomalies

Li, Linghan

2013-01-01T23:59:59.000Z

492

NOAA Technical Memorandum GLERL-135 Great Lakes Ice Cover Climatology  

E-Print Network [OSTI]

____________________________________________________________________________ Great Lakes Ice Cover Climatology Update: Winters 2003, 2004, and 2005 Raymond A. Assel NOAA, Great..................................................................................................6 DATES OF FIRST (LAST) ICE AND ICE DURATION. .............................................................7 SEASONAL PROGRESSION OF ICE COVER

493

Thermal Storage with Ice Harvesting Systems  

E-Print Network [OSTI]

Application of Harvesting Ice Storage Systems. Thermal storage systems are becoming widely accepted techniques for utility load management. This paper discusses the principles of ice harvesting equipment and their application to the multi...

Knebel, D. E.

1986-01-01T23:59:59.000Z

494

Quantum Ice : a quantum Monte Carlo study  

E-Print Network [OSTI]

Ice states, in which frustrated interactions lead to a macroscopic ground-state degeneracy, occur in water ice, in problems of frustrated charge order on the pyrochlore lattice, and in the family of rare-earth magnets collectively known as spin ice. Of particular interest at the moment are "quantum spin ice" materials, where large quantum fluctuations may permit tunnelling between a macroscopic number of different classical ground states. Here we use zero-temperature quantum Monte Carlo simulations to show how such tunnelling can lift the degeneracy of a spin or charge ice, stabilising a unique "quantum ice" ground state --- a quantum liquid with excitations described by the Maxwell action of 3+1-dimensional quantum electrodynamics. We further identify a competing ordered "squiggle" state, and show how both squiggle and quantum ice states might be distinguished in neutron scattering experiments on a spin ice material.

Nic Shannon; Olga Sikora; Frank Pollmann; Karlo Penc; Peter Fulde

2011-12-13T23:59:59.000Z

495

Heavy ion irradiation of crystalline water ice  

E-Print Network [OSTI]

Under cosmic irradiation, the interstellar water ice mantles evolve towards a compact amorphous state. Crystalline ice amorphisation was previously monitored mainly in the keV to hundreds of keV ion energies. We experimentally investigate heavy ion irradiation amorphisation of crystalline ice, at high energies closer to true cosmic rays, and explore the water-ice sputtering yield. We irradiated thin crystalline ice films with MeV to GeV swift ion beams, produced at the GANIL accelerator. The ice infrared spectral evolution as a function of fluence is monitored with in-situ infrared spectroscopy (induced amorphisation of the initial crystalline state into a compact amorphous phase). The crystalline ice amorphisation cross-section is measured in the high electronic stopping-power range for different temperatures. At large fluence, the ice sputtering is measured on the infrared spectra, and the fitted sputtering-yield dependence, combined with previous measurements, is quadratic over three decades of electronic ...

Dartois, E; Boduch, P; Brunetto, R; Chabot, M; Domaracka, A; Ding, J J; Kamalou, O; Lv, X Y; Rothard, H; da Silveira, E F; Thomas, J C

2015-01-01T23:59:59.000Z

496

Quenched by ice: Transient grating measurements of vibronic dynamics in bromine-doped ice  

E-Print Network [OSTI]

Quenched by ice: Transient grating measurements of vibronic dynamics in bromine-doped ice I. U April 2006; published online 25 May 2006 In both water and in ice, the absorption spectra of bromine of the trapped molecule in its electronic B 3 0u state in ice. Independent of the initial excitation energy

Apkarian, V. Ara

497

Sea ice control of water isotope transport to Antarctica and implications for ice core interpretation  

E-Print Network [OSTI]

associated with diabatic heating. The interior deuterium excess response is more strongly affected by sea ice ice and the local conditions may have remote influences [Jacobs and Comiso, 1997; StammerjohnSea ice control of water isotope transport to Antarctica and implications for ice core

Noone, David

498

New study details glacier ice loss following ice shelf July 25, 2011  

E-Print Network [OSTI]

and Ted #12;Scambos of the NSIDC produced detailed ice loss maps from 2001 to 2009 for the main tributaryNew study details glacier ice loss following ice shelf collapse July 25, 2011 Contact: Anthony Lane UMBC (410) 455-5793 alane@umbc.edu Katherine Leitzell National Snow and Ice Data Center University

Cambridge, University of

499

Ice Sample Production Techniques and Indentation Tests for Laboratory Experiments Simulating Ship Collisions with Ice  

E-Print Network [OSTI]

questions involving the fracture of ice. METHODS For STePS2 investigations ice is variously produced usingIce Sample Production Techniques and Indentation Tests for Laboratory Experiments Simulating Ship Collisions with Ice Stephen E. Bruneau1 , Anna K. Dillenburg2 , and Simon Ritter2 1 Prof. of Civil

Bruneau, Steve

500

LABORATORY INDENTATION TESTS SIMULATING ICE-STRUCTURE INTERACTIONS USING CONE-SHAPED ICE  

E-Print Network [OSTI]

involving closing speeds over 1500m/s. Ice was produced using distilled and chilled water, unLABORATORY INDENTATION TESTS SIMULATING ICE- STRUCTURE INTERACTIONS USING CONE-SHAPED ICE SAMPLES describes the results of a series of tests from 2010-2012 in which cone-shaped ice samples were crushed

Bruneau, Steve