Articles | Volume 13, issue 7
https://doi.org/10.5194/tc-13-1911-2019
https://doi.org/10.5194/tc-13-1911-2019
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, Alexander Robinson, Jorge Alvarez-Solas, and Marisa Montoya

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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.