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|a (TOE)ost971306
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|a (TOE)971306
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|a E 1.99: la-ur-09-6177
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|a E 1.99:la-ur-09-06177
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|a E 1.99: la-ur-09-6177
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|a la-ur-09-6177
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|a la-ur-09-06177
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|a Greenland ice sheet surface mass-balance modeling in a 131-year perspective, 1950-2080
|h [electronic resource]
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| 260 |
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|a Washington, D.C. :
|b United States. Department of Energy ;
|a Oak Ridge, Tenn. :
|b distributed by the Office of Scientific and Technical Information, U.S. Department of Energy,
|c 2009.
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| 336 |
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|a text
|b txt
|2 rdacontent.
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| 337 |
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|a computer
|b c
|2 rdamedia.
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| 338 |
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|a online resource
|b cr
|2 rdacarrier.
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|a Published through SciTech Connect.
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| 500 |
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|a 01/01/2009.
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|a "la-ur-09-06177"
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| 500 |
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|a " la-ur-09-6177"
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| 500 |
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|a Journal of Hydrometeorology FT.
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| 500 |
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|a Christensen, Jens; Liston, Glen; Mernild, Sebastian Haugard; Hiemstra, Christopher.
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| 520 |
3 |
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|a 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 ≈90% increase in end-of-summer surface melt extent (0.483 x 10⁶ km²) from 1950 to 2080, and a melt index (above 2,000-m elevation) increase of 138% (1.96 x 10⁶ km² 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 (≈50-70%) and was lowest in the west (≈20-30%). The rate of SMB loss, largely tied to changes in ablation processes, lead to an enhanced average loss of 331 km³ from 1950 to 2080, an average 5MB level of -99 km³ 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⁻¹. The accumulated GrIS freshwater runoff contribution from surface melting equaled 160 mm SLE from 1950 through 2080.
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|b AC52-06NA25396.
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| 650 |
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|a Ablation.
|2 local.
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| 650 |
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|a Boundary Conditions.
|2 local.
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| 650 |
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|a Climates.
|2 local.
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| 650 |
|
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|a Fluctuations.
|2 local.
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| 650 |
|
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|a Greenland.
|2 local.
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| 650 |
|
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|a Mass Balance.
|2 local.
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| 650 |
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|a Melting.
|2 local.
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| 650 |
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7 |
|a Runoff.
|2 local.
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| 650 |
|
7 |
|a Sea Level.
|2 local.
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| 650 |
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|a Simulation.
|2 local.
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| 650 |
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|a Surface Waters.
|2 local.
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| 650 |
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|a Satellites.
|2 local.
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| 650 |
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|a Wmo.
|2 local.
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| 710 |
2 |
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|a Los Alamos National Laboratory.
|4 res.
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| 710 |
1 |
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|a United States.
|b Department of Energy.
|4 spn.
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| 710 |
1 |
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|a United States.
|b Department of Energy.
|b Office of Scientific and Technical Information.
|4 dst.
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| 856 |
4 |
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|u http://www.osti.gov/servlets/purl/971306/
|z Online Access
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| 907 |
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|a .b7059613x
|b 03-07-23
|c 04-03-12
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| 998 |
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|a web
|b 04-03-12
|c f
|d m
|e p
|f eng
|g
|h 0
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|s ae649745-d146-596e-94cd-c4ff0f65ea9a
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| 952 |
f |
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|p Can circulate
|a University of Colorado Boulder
|b Online
|c Online
|d Online
|e E 1.99: la-ur-09-6177
|h Superintendent of Documents classification
|i web
|n 1
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