Articles | Volume 13, issue 10
https://doi.org/10.5194/tc-13-2615-2019
https://doi.org/10.5194/tc-13-2615-2019
Research article
 | 
09 Oct 2019
Research article |  | 09 Oct 2019

Nonlinear response of the Antarctic Ice Sheet to late Quaternary sea level and climate forcing

Michelle Tigchelaar, Axel Timmermann, Tobias Friedrich, Malte Heinemann, and David Pollard

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (02 Sep 2019) by Jan De Rydt
AR by Michelle Tigchelaar on behalf of the Authors (04 Sep 2019)  Author's response   Manuscript 
ED: Publish as is (09 Sep 2019) by Jan De Rydt
AR by Michelle Tigchelaar on behalf of the Authors (10 Sep 2019)
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Short summary
The Antarctic Ice Sheet has expanded and retracted often in the past, but, so far, studies have not identified which environmental driver is most important: air temperature, snowfall, ocean conditions or global sea level. In a modeling study of 400 000 years of Antarctic Ice Sheet variability we isolated different drivers and found that no single driver dominates. Air temperature and sea level are most important and combine in a synergistic way, with important implications for future change.