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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 3
The Cryosphere, 9, 1005-1024, 2015
https://doi.org/10.5194/tc-9-1005-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 9, 1005-1024, 2015
https://doi.org/10.5194/tc-9-1005-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 13 May 2015

Research article | 13 May 2015

Oceanic and atmospheric forcing of Larsen C Ice-Shelf thinning

P. R. Holland et al.
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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR by Paul Holland on behalf of the Authors (24 Mar 2015)  Author's response    Manuscript
ED: Publish as is (27 Mar 2015) by Olivier Gagliardini
Publications Copernicus
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Short summary
Antarctic Peninsula ice shelves have collapsed in recent decades. The surface of Larsen C Ice Shelf is lowering, but the cause of this has not been understood. This study uses eight radar surveys to show that the lowering is caused by both ice loss and a loss of air from the ice shelf's snowpack. At least two different processes are causing the lowering. The stability of Larsen C may be at risk from an ungrounding of Bawden Ice Rise or ice-front retreat past a 'compressive arch' in strain rates.
Antarctic Peninsula ice shelves have collapsed in recent decades. The surface of Larsen C Ice...
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