Articles | Volume 11, issue 4
https://doi.org/10.5194/esd-11-1153-2020
https://doi.org/10.5194/esd-11-1153-2020
Research article
 | 
16 Dec 2020
Research article |  | 16 Dec 2020

Future sea level contribution from Antarctica inferred from CMIP5 model forcing and its dependence on precipitation ansatz

Christian B. Rodehacke, Madlene Pfeiffer, Tido Semmler, Özgür Gurses, and Thomas Kleiner

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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 Apr 2020) by Yun Liu
AR by Anna Wenzel on behalf of the Authors (30 Apr 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (06 May 2020) by Yun Liu
RR by Anonymous Referee #2 (20 May 2020)
RR by Anonymous Referee #3 (04 Aug 2020)
ED: Reconsider after major revisions (12 Aug 2020) by Yun Liu
AR by Christian Rodehacke on behalf of the Authors (23 Sep 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (30 Sep 2020) by Yun Liu
RR by Anonymous Referee #2 (12 Oct 2020)
RR by Anonymous Referee #3 (19 Oct 2020)
ED: Publish subject to minor revisions (review by editor) (19 Oct 2020) by Yun Liu
AR by Christian Rodehacke on behalf of the Authors (27 Oct 2020)  Author's response    Manuscript
ED: Publish as is (06 Nov 2020) by Yun Liu
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Short summary
In the warmer future, Antarctica's ice sheet will lose more ice due to enhanced iceberg calving and a warming ocean that melts more floating ice from below. However, the hydrological cycle is also stronger in a warmer world. Hence, more snowfall will precipitate on Antarctica and may balance the amplified ice loss. We have used future climate scenarios from various global climate models to perform numerous ice sheet simulations to show that precipitation may counteract mass loss.
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