Journal cover Journal topic
Climate of the Past An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

IF value: 3.536
IF3.536
IF 5-year value: 3.967
IF 5-year
3.967
CiteScore value: 6.6
CiteScore
6.6
SNIP value: 1.262
SNIP1.262
IPP value: 3.90
IPP3.90
SJR value: 2.185
SJR2.185
Scimago H <br class='widget-line-break'>index value: 71
Scimago H
index
71
h5-index value: 40
h5-index40
CP | Articles | Volume 14, issue 4
Clim. Past, 14, 455–472, 2018
https://doi.org/10.5194/cp-14-455-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Clim. Past, 14, 455–472, 2018
https://doi.org/10.5194/cp-14-455-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 09 Apr 2018

Research article | 09 Apr 2018

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

Ilaria Tabone et al.

Download

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
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 Bas de Boer (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
Publications Copernicus
Download
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.
The response of the Greenland Ice Sheet (GrIS) to palaeo-oceanic changes on a...
Citation