Articles | Volume 14, issue 4
https://doi.org/10.5194/cp-14-455-2018
https://doi.org/10.5194/cp-14-455-2018
Research article
 | 
09 Apr 2018
Research article |  | 09 Apr 2018

The sensitivity of the Greenland Ice Sheet to glacial–interglacial oceanic forcing

Ilaria Tabone, Javier Blasco, Alexander Robinson, Jorge Alvarez-Solas, and Marisa Montoya

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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: Reconsider after major revisions (03 Feb 2018) by Alessio Rovere
AR by Ilaria Tabone on behalf of the Authors (13 Feb 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (14 Feb 2018) by Alessio Rovere
RR by (26 Feb 2018)
ED: Publish subject to minor revisions (review by editor) (02 Mar 2018) by Alessio Rovere
AR by Ilaria Tabone on behalf of the Authors (09 Mar 2018)  Author's response   Manuscript 
ED: Publish as is (13 Mar 2018) by Alessio Rovere
AR by Ilaria Tabone on behalf of the Authors (19 Mar 2018)  Manuscript 
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Short summary
The response of the Greenland Ice Sheet (GrIS) to palaeo-oceanic changes on a glacial–interglacial timescale is studied from a modelling perspective. A 3-D hybrid ice-sheet–shelf model which includes a parameterization of the basal melting rate at the GrIS marine margins is used. The results show that the oceanic forcing plays a key role in the GrIS evolution, not only by controlling the ice retreat during the deglaciation but also by driving the ice expansion in glacial periods.