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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, 881–903, 2015
https://doi.org/10.5194/tc-9-881-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 9, 881–903, 2015
https://doi.org/10.5194/tc-9-881-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 06 May 2015

Research article | 06 May 2015

Simulating the Antarctic ice sheet in the late-Pliocene warm period: PLISMIP-ANT, an ice-sheet model intercomparison project

B. de Boer et al.
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Interactive discussion
Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Bas de Boer on behalf of the Authors (14 Feb 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (17 Feb 2015) by G. Hilmar Gudmundsson
RR by Stephen Cornford (06 Mar 2015)
RR by Anonymous Referee #2 (05 Apr 2015)
ED: Publish as is (16 Apr 2015) by G. Hilmar Gudmundsson
AR by Bas de Boer on behalf of the Authors (24 Apr 2015)  Author's response    Manuscript
Publications Copernicus
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Short summary
We present results from simulations of the Antarctic ice sheet by means of an intercomparison project with six ice-sheet models. Our results demonstrate the difficulty of all models used here to simulate a significant retreat or re-advance of the East Antarctic ice grounding line. Improved grounding-line physics could be essential for a correct representation of the migration of the grounding line of the Antarctic ice sheet during the Pliocene.
We present results from simulations of the Antarctic ice sheet by means of an intercomparison...
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