Articles | Volume 11, issue 12
https://doi.org/10.5194/gmd-11-5003-2018
https://doi.org/10.5194/gmd-11-5003-2018
Model description paper
 | 
07 Dec 2018
Model description paper |  | 07 Dec 2018

The GRISLI ice sheet model (version 2.0): calibration and validation for multi-millennial changes of the Antarctic ice sheet

Aurélien Quiquet, Christophe Dumas, Catherine Ritz, Vincent Peyaud, and Didier M. Roche

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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 Aurélien Quiquet on behalf of the Authors (07 Sep 2018)  Author's response    Manuscript
ED: Reconsider after major revisions (23 Oct 2018) by Julia Hargreaves
AR by Aurélien Quiquet on behalf of the Authors (30 Oct 2018)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (14 Nov 2018) by Julia Hargreaves
AR by Aurélien Quiquet on behalf of the Authors (19 Nov 2018)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (22 Nov 2018) by Julia Hargreaves
AR by Aurélien Quiquet on behalf of the Authors (23 Nov 2018)  Author's response    Manuscript
ED: Publish as is (27 Nov 2018) by Julia Hargreaves
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Short summary
This paper presents the GRISLI (Grenoble ice sheet and land ice) model in its newest revision. We present the recent model improvements from its original version (Ritz et al., 2001), together with a discussion of the model performance in reproducing the present-day Antarctic ice sheet geometry and the grounding line advances and retreats during the last 400 000 years. We show that GRISLI is a computationally cheap model, able to reproduce the large-scale behaviour of ice sheets.