Articles | Volume 11, issue 5
The Cryosphere, 11, 2213–2229, 2017
https://doi.org/10.5194/tc-11-2213-2017
The Cryosphere, 11, 2213–2229, 2017
https://doi.org/10.5194/tc-11-2213-2017

Research article 18 Sep 2017

Research article | 18 Sep 2017

Regional modeling of the Shirase drainage basin, East Antarctica: full Stokes vs. shallow ice dynamics

Hakime Seddik et al.

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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 Hakime SEDDIK on behalf of the Authors (06 Mar 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (17 Mar 2017) by Eric Larour
RR by Anonymous Referee #3 (02 Apr 2017)
RR by Anonymous Referee #4 (25 Apr 2017)
ED: Publish subject to minor revisions (Editor review) (06 Jul 2017) by Eric Larour
AR by Anna Wenzel on behalf of the Authors (11 Jul 2017)  Author's response    Manuscript
ED: Publish as is (11 Aug 2017) by Eric Larour
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Short summary
The Shirase Glacier in Antarctica is studied by means of a computer model. This model implements two physical approaches to represent the glacier flow dynamics. This study finds that it is important to use the more precise and sophisticated method in order to better understand and predict the evolution of fast flowing glaciers. This may be important to more accurately predict the sea level change due to global warming.