Articles | Volume 16, issue 6
https://doi.org/10.5194/cp-16-2275-2020
https://doi.org/10.5194/cp-16-2275-2020
Research article
 | 
20 Nov 2020
Research article |  | 20 Nov 2020

Contribution of the coupled atmosphere–ocean–sea ice–vegetation model COSMOS to the PlioMIP2

Christian Stepanek, Eric Samakinwa, Gregor Knorr, and Gerrit Lohmann

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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: Publish subject to minor revisions (review by editor) (03 May 2020) by Wing-Le Chan
AR by Christian Stepanek on behalf of the Authors (25 May 2020)
ED: Publish subject to minor revisions (review by editor) (18 Jun 2020) by Wing-Le Chan
AR by Christian Stepanek on behalf of the Authors (26 Jun 2020)  Author's response   Manuscript 
ED: Publish subject to technical corrections (07 Jul 2020) by Wing-Le Chan
AR by Christian Stepanek on behalf of the Authors (10 Jul 2020)  Manuscript 
Short summary
Future climate is expected to be warmer than today. We study climate based on simulations of the mid-Pliocene (about 3 million years ago), which was a time of elevated temperatures, and discuss implications for the future. Our results are provided towards a comparison to both proxy evidence and output of other climate models. We simulate a mid-Pliocene climate that is both warmer and wetter than today. Some climate characteristics can be more directly transferred to the near future than others.