The role of ocean and atmospheric dynamics in the marine-based collapse of the last Eurasian Ice Sheet
The last deglaciation of the marine parts of the Eurasian Ice Sheet was driven mainly by oceanic temperature change in the north and by changes in solar insolation in the south, based on a reconstruction of the marine parts of the Eurasian Ice Sheet and Nordic Seas palaeoceanographic data.
| Main Authors: | , , , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2022-05-01
|
| Series: | Communications Earth & Environment |
| Online Access: | https://doi.org/10.1038/s43247-022-00447-0 |