Articles | Volume 12, issue 7
https://doi.org/10.5194/tc-12-2383-2018
https://doi.org/10.5194/tc-12-2383-2018
Research article
 | 
20 Jul 2018
Research article |  | 20 Jul 2018

Deglaciation and future stability of the Coats Land ice margin, Antarctica

Dominic A. Hodgson, Kelly Hogan, James M. Smith, James A. Smith, Claus-Dieter Hillenbrand, Alastair G. C. Graham, Peter Fretwell, Claire Allen, Vicky Peck, Jan-Erik Arndt, Boris Dorschel, Christian Hübscher, Andrew M. Smith, and Robert Larter

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Dominic Hodgson on behalf of the Authors (14 May 2018)  Author's response   Manuscript 
ED: Publish as is (18 May 2018) by Chris R. Stokes
AR by Dominic Hodgson on behalf of the Authors (07 Jun 2018)  Manuscript 

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Dominic Hodgson on behalf of the Authors (10 Jul 2018)   Author's adjustment   Manuscript
EA: Adjustments approved (12 Jul 2018) by Chris R. Stokes
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Short summary
We studied the Coats Land ice margin, Antarctica, providing a multi-disciplinary geophysical assessment of the ice sheet configuration through its last advance and retreat; a description of the physical constraints on the stability of the past and present ice and future margin based on its submarine geomorphology and ice-sheet geometry; and evidence that once detached from the bed, the ice shelves in this region were predisposed to rapid retreat back to coastal grounding lines.