Contribution of the Greenland Ice Sheet to sea level over the next millennium

Author:

Aschwanden Andy1ORCID,Fahnestock Mark A.1ORCID,Truffer Martin1,Brinkerhoff Douglas J.2,Hock Regine1,Khroulev Constantine1ORCID,Mottram Ruth3ORCID,Khan S. Abbas4ORCID

Affiliation:

1. University of Alaska Fairbanks, 2156 Koyukuk Dr., Fairbanks, AK 99775, USA.

2. Computer Science Department, University of Missoula, Missoula, MT 59812, USA.

3. Danish Meteorological Institute, Copenhagen, Denmark.

4. DTU Space, Kongens Lyngby, Denmark.

Abstract

Simulations show that the Greenland Ice Sheet could disappear within a millennium if greenhouse gas emissions continue unabated.

Funder

National Science Foundation

National Aeronautics and Space Administration

Carlsbergfondet

Danish Council for Independent Research

European Research Council

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference61 articles.

1. Seasonal to decadal variability in ice discharge from the Greenland Ice Sheet;King M. D.;Cryosphere,2018

2. The influence of North Atlantic atmospheric and oceanic forcing effects on 1900−2010 Greenland summer climate and ice melt/runoff;Hanna E.;Int. J. Climatol.,2013

3. Acceleration of Jakobshavn Isbræ triggered by warm subsurface ocean waters

4. Seasonal to decadal scale variations in the surface velocity of Jakobshavn Isbrae, Greenland: Observation and model-based analysis;Joughin I.;J. Geophys. Res.,2012

5. Large fluctuations in speed on Greenland’s Jakobshavn Isbræ glacier;Joughin I.;Nature,2004

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