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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 13, issue 9
Clim. Past, 13, 1243–1257, 2017
https://doi.org/10.5194/cp-13-1243-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 13, 1243–1257, 2017
https://doi.org/10.5194/cp-13-1243-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 25 Sep 2017

Research article | 25 Sep 2017

The influence of ice sheets on temperature during the past 38 million years inferred from a one-dimensional ice sheet–climate model

Lennert B. Stap et al.

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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 (16 Mar 2017) by Zhengtang Guo
AR by Lennert Stap on behalf of the Authors (26 Apr 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (30 Apr 2017) by Zhengtang Guo
RR by Anonymous Referee #1 (22 May 2017)
RR by Anonymous Referee #3 (08 Jun 2017)
RR by Anonymous Referee #4 (21 Jun 2017)
RR by Anonymous Referee #2 (03 Jul 2017)
ED: Publish subject to minor revisions (review by Editor) (11 Jul 2017) by Zhengtang Guo
AR by Lennert Stap on behalf of the Authors (21 Aug 2017)  Author's response    Manuscript
ED: Publish as is (23 Aug 2017) by Zhengtang Guo
AR by Lennert Stap on behalf of the Authors (23 Aug 2017)  Author's response    Manuscript
Publications Copernicus
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Short summary
We show the results of transient simulations with a coupled climate–ice sheet model over the past 38 million years. The CO2 forcing of the model is inversely obtained from a benthic δ18O stack. These simulations enable us to study the influence of ice sheet variability on climate change on long timescales. We find that ice sheet–climate interaction strongly enhances Earth system sensitivity and polar amplification.
We show the results of transient simulations with a coupled climate–ice sheet model over the...
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