Oceanic response to changes in the WAIS and astronomical forcing during the MIS31 superinterglacial
Marine Isotope Stage 31 (MIS31, between 1085 and 1055 ka) was characterized by higher extratropical air temperatures and a substantial recession of polar glaciers compared to today. Paleoreconstructions and model simulations have increased the understanding of the MIS31 interval, but questions r...
| Main Authors: | , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2017-09-01
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| Series: | Climate of the Past |
| Online Access: | https://www.clim-past.net/13/1081/2017/cp-13-1081-2017.pdf |