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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 6, issue 6
The Cryosphere, 6, 1239-1250, 2012
https://doi.org/10.5194/tc-6-1239-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 6, 1239-1250, 2012
https://doi.org/10.5194/tc-6-1239-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 05 Nov 2012

Research article | 05 Nov 2012

Melting of Northern Greenland during the last interglaciation

A. Born1,2 and K. H. Nisancioglu3,4 A. Born and K. H. Nisancioglu
  • 1Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
  • 2Oeschger Centre for Climate Change Research, Bern, Switzerland
  • 3Bjerknes Centre for Climate Research, University of Bergen, Bergen, Norway
  • 4UNI Research, Bergen, Norway

Abstract. Using simulated climate data from the comprehensive coupled climate model IPSL CM4, we simulate the Greenland ice sheet (GrIS) during the Eemian interglaciation with the three-dimensional ice sheet model SICOPOLIS. The Eemian is a period 126 000 yr before present (126 ka) with Arctic temperatures comparable to projections for the end of this century. In our simulation, the northeastern part of the GrIS is unstable and retreats significantly, despite moderate melt rates. This result is found to be robust to perturbations within a wide parameter space of key parameters of the ice sheet model, the choice of initial ice temperature, and has been reproduced with climate forcing from a second coupled climate model, the CCSM3. It is shown that the northeast GrIS is the most vulnerable. Even a small increase in melt removes many years of ice accumulation, giving a large mass imbalance and triggering the strong ice-elevation feedback. Unlike the south and west, melting in the northeast is not compensated by high accumulation. The analogy with modern warming suggests that in coming decades, positive feedbacks could increase the rate of mass loss of the northeastern GrIS, exceeding the recent observed thinning rates in the south.

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