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The Cryosphere An interactive open-access journal of the European Geosciences Union
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TC | Articles | Volume 13, issue 7
The Cryosphere, 13, 1911–1923, 2019
https://doi.org/10.5194/tc-13-1911-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 13, 1911–1923, 2019
https://doi.org/10.5194/tc-13-1911-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 15 Jul 2019

Research article | 15 Jul 2019

Submarine melt as a potential trigger of the North East Greenland Ice Stream margin retreat during Marine Isotope Stage 3

Ilaria Tabone 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
AR by Ilaria Tabone on behalf of the Authors (26 Apr 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (10 May 2019) by Andreas Vieli
RR by Anonymous Referee #3 (16 Jun 2019)
ED: Publish subject to technical corrections (20 Jun 2019) by Andreas Vieli
Publications Copernicus
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Short summary
Recent reconstructions show that the North East Greenland Ice Stream (NEGIS) retreated away from its present-day position by 20–40 km during MIS-3. Atmospheric and external forcings were proposed as potential causes of this retreat, but the role of the ocean was not considered. Here, using a 3-D ice-sheet model, we suggest that oceanic warming is sufficient to induce a retreat of the NEGIS margin of many tens of kilometres during MIS-3, helping to explain this conundrum.
Recent reconstructions show that the North East Greenland Ice Stream (NEGIS) retreated away from...
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