The Cryosphere
The Cryosphere
TC
Articles | Volume 13, issue 8
Articles | Volume 13, issue 8
https://doi.org/10.5194/tc-13-2133-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-13-2133-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 13, issue 8
Research article
 | 
15 Aug 2019
Research article |  | 15 Aug 2019

Eemian Greenland ice sheet simulated with a higher-order model shows strong sensitivity to surface mass balance forcing

Andreas Plach, Kerim H. Nisancioglu, Petra M. Langebroek, Andreas Born, and Sébastien Le clec'h

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Latest update: 19 Nov 2024
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Short summary
Meltwater from the Greenland ice sheet (GrIS) rises sea level and knowing how the GrIS behaved in the past will help to become better in predicting its future. Here, the evolution of the past GrIS is shown to be dominated by how much ice melts (a result of the prevailing climate) rather than how ice flow is represented in the simulations. Therefore, it is very important to know past climates accurately, in order to be able to simulate the evolution of the GrIS and its contribution to sea level.
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