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.

Bibliographic Details
Published in:Communications Earth & Environment
Main Authors: Hans Petter Sejrup, Berit Oline Hjelstuen, Henry Patton, Mariana Esteves, Monica Winsborrow, Tine Lander Rasmussen, Karin Andreassen, Alun Hubbard
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2022
Subjects:
Geology
QE1-996.5
Environmental sciences
GE1-350
Ice Sheet
Nordic Seas
Online Access:https://doi.org/10.1038/s43247-022-00447-0
https://doaj.org/article/aa393b2bc73f47e494875ae8c1613ed3
Description
Summary: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.

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