Articles | Volume 14, issue 3
https://doi.org/10.5194/tc-14-985-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/tc-14-985-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Twenty-first century ocean forcing of the Greenland ice sheet for modelling of sea level contribution
Scripps Institution of Oceanography, University of California San Diego, La Jolla, California, USA
Denis Felikson
Cryospheric Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
Fiamma Straneo
Scripps Institution of Oceanography, University of California San Diego, La Jolla, California, USA
Heiko Goelzer
Institute for Marine and Atmospheric research Utrecht, Utrecht University, Utrecht, the Netherlands
Laboratoire de Glaciologie, Université Libre de Bruxelles, Brussels, Belgium
Christopher M. Little
Atmospheric and Environmental Research, Inc., Lexington, Massachusetts, USA
Mathieu Morlighem
Department of Earth System Science, University of California, Irvine, California, USA
Xavier Fettweis
Laboratory of Climatology, SPHERES research unit, University of Liège, Liège, Belgium
Sophie Nowicki
Cryospheric Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
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- The future sea-level contribution of the Greenland ice sheet: a multi-model ensemble study of ISMIP6 H. Goelzer et al. 10.5194/tc-14-3071-2020
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- Coupling the U.K. Earth System Model to Dynamic Models of the Greenland and Antarctic Ice Sheets R. Smith et al. 10.1029/2021MS002520
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- Estimating Greenland tidewater glacier retreat driven by submarine melting D. Slater et al. 10.5194/tc-13-2489-2019
- Reduced Ice Loss From Greenland Under Stratospheric Aerosol Injection J. Moore et al. 10.1029/2023JF007112
Latest update: 12 Nov 2024
Short summary
Changes in the ocean around Greenland play an important role in determining how much the ice sheet will contribute to global sea level over the coming century. However, capturing these links in models is very challenging. This paper presents a strategy enabling an ensemble of ice sheet models to feel the effect of the ocean for the first time and should therefore result in a significant improvement in projections of the Greenland ice sheet's contribution to future sea level change.
Changes in the ocean around Greenland play an important role in determining how much the ice...
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