Articles | Volume 13, issue 10
The Cryosphere, 13, 2615–2631, 2019
The Cryosphere, 13, 2615–2631, 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 et al.


Interactive discussion

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) (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
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.