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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, 1497-1505, 2012
https://doi.org/10.5194/tc-6-1497-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 6, 1497-1505, 2012
https://doi.org/10.5194/tc-6-1497-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 12 Dec 2012

Research article | 12 Dec 2012

The stability of grounding lines on retrograde slopes

G. H. Gudmundsson1, J. Krug2, G. Durand2, L. Favier2, and O. Gagliardini2,3 G. H. Gudmundsson et al.
  • 1British Antarctic Survey, High Cross, Madingley Rd., Cambridge, CB3 0ET, UK
  • 2Laboratoire de Glaciologie et Géophysique de l'Environnement, UJF-Grenoble, CNRS, Saint-Martin-d'Hères, France
  • 3Institut Universitaire de France, 103, BD Saint-Michel, 75005 Paris, France

Abstract. The stability of marine ice sheets grounded on beds that slope upwards in the overall direction of flow is investigated numerically in two horizontal dimensions. We give examples of stable grounding lines on such retrograde slopes illustrating that marine ice sheets are not unconditionally unstable in two horizontal dimensions. Retrograde bed slopes at the grounding lines of marine ice sheets, such as the West Antarctic Ice Sheet (WAIS), do not per se imply an instability, nor do they imply that these regions are close to a threshold of instability. We therefore question those estimates of the potential near-future contribution of WAIS to global sea level change based solely on the notion that WAIS, resting on a retrograde slope, must be inherently unstable.

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