Articles | Volume 15, issue 2
The Cryosphere, 15, 1031–1052, 2021
https://doi.org/10.5194/tc-15-1031-2021

Special issue: The Ice Sheet Model Intercomparison Project for CMIP6...

The Cryosphere, 15, 1031–1052, 2021
https://doi.org/10.5194/tc-15-1031-2021

Research article 26 Feb 2021

Research article | 26 Feb 2021

The GRISLI-LSCE contribution to the Ice Sheet Model Intercomparison Project for phase 6 of the Coupled Model Intercomparison Project (ISMIP6) – Part 2: Projections of the Antarctic ice sheet evolution by the end of the 21st century

Aurélien Quiquet and Christophe Dumas

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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
ED: Publish subject to revisions (further review by editor and referees) (13 Nov 2020) by Ayako Abe-Ouchi
AR by Aurélien Quiquet on behalf of the Authors (13 Nov 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (14 Nov 2020) by Ayako Abe-Ouchi
RR by Fuyuki SAITO (07 Dec 2020)
RR by Johannes Sutter (08 Dec 2020)
ED: Publish subject to revisions (further review by editor and referees) (21 Dec 2020) by Ayako Abe-Ouchi
AR by Aurélien Quiquet on behalf of the Authors (21 Jan 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to technical corrections (29 Jan 2021) by Ayako Abe-Ouchi
AR by Aurélien Quiquet on behalf of the Authors (01 Feb 2021)  Author's response    Manuscript
Short summary
We present here the GRISLI-LSCE contribution to the Ice Sheet Model Intercomparison Project for CMIP6 for Antarctica. The project aims to quantify the ice sheet contribution to global sea level rise for the next century. We show that increased precipitation in the future in some cases mitigates this contribution, with positive to negative values in 2100 depending of the climate forcing used. Sub-shelf-basal-melt uncertainties induce large differences in simulated grounding-line retreats.