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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 7 | Copyright
The Cryosphere, 12, 2307-2326, 2018
https://doi.org/10.5194/tc-12-2307-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 19 Jul 2018

Research article | 19 Jul 2018

Dynamic response of Antarctic Peninsula Ice Sheet to potential collapse of Larsen C and George VI ice shelves

Clemens Schannwell et al.
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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Clemens Schannwell on behalf of the Authors (09 May 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (18 May 2018) by Olivier Gagliardini
RR by Anonymous Referee #1 (25 May 2018)
RR by Anonymous Referee #2 (05 Jun 2018)
ED: Publish subject to minor revisions (review by editor) (05 Jun 2018) by Olivier Gagliardini
AR by Clemens Schannwell on behalf of the Authors (18 Jun 2018)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (21 Jun 2018) by Olivier Gagliardini
AR by Lorena Grabowski on behalf of the Authors (26 Jun 2018)  Author's response
ED: Publish subject to technical corrections (26 Jun 2018) by Olivier Gagliardini
Publications Copernicus
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Short summary
Despite the speculation on the state and fate of Larsen C Ice Shelf, a key unknown factor remains: what would be the effects of ice-shelf collapse on upstream drainage basins and thus global sea levels? In our paper three state-of-the-art numerical ice-sheet models were used to simulate the volume evolution of the inland ice sheet to ice-shelf collapse at Larsen C and George VI ice shelves. Our results suggest sea-level rise of up to ~ 4 mm for Larsen C ice shelf and ~ 22 for George VI ice shelf.
Despite the speculation on the state and fate of Larsen C Ice Shelf, a key unknown factor...
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