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
Main Authors: Hans Petter Sejrup, Berit Oline Hjelstuen, Henry Patton, Mariana Esteves, Monica Winsborrow, Tine Lander Rasmussen, Karin Andreassen, Alun Hubbard
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
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author Hans Petter Sejrup
Berit Oline Hjelstuen
Henry Patton
Mariana Esteves
Monica Winsborrow
Tine Lander Rasmussen
Karin Andreassen
Alun Hubbard
author_facet Hans Petter Sejrup
Berit Oline Hjelstuen
Henry Patton
Mariana Esteves
Monica Winsborrow
Tine Lander Rasmussen
Karin Andreassen
Alun Hubbard
author_sort Hans Petter Sejrup
collection DOAJ
description 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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spelling doaj.art-aa393b2bc73f47e494875ae8c1613ed32022-12-22T00:23:23ZengNature PortfolioCommunications Earth & Environment2662-44352022-05-013111010.1038/s43247-022-00447-0The role of ocean and atmospheric dynamics in the marine-based collapse of the last Eurasian Ice SheetHans Petter Sejrup0Berit Oline Hjelstuen1Henry Patton2Mariana Esteves3Monica Winsborrow4Tine Lander Rasmussen5Karin Andreassen6Alun Hubbard7Department of Earth Science, University of BergenDepartment of Earth Science, University of BergenCentre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT the Arctic University of NorwayCentre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT the Arctic University of NorwayCentre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT the Arctic University of NorwayCentre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT the Arctic University of NorwayCentre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT the Arctic University of NorwayCentre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT the Arctic University of NorwayThe 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.https://doi.org/10.1038/s43247-022-00447-0
spellingShingle Hans Petter Sejrup
Berit Oline Hjelstuen
Henry Patton
Mariana Esteves
Monica Winsborrow
Tine Lander Rasmussen
Karin Andreassen
Alun Hubbard
The role of ocean and atmospheric dynamics in the marine-based collapse of the last Eurasian Ice Sheet
Communications Earth & Environment
title The role of ocean and atmospheric dynamics in the marine-based collapse of the last Eurasian Ice Sheet
title_full The role of ocean and atmospheric dynamics in the marine-based collapse of the last Eurasian Ice Sheet
title_fullStr The role of ocean and atmospheric dynamics in the marine-based collapse of the last Eurasian Ice Sheet
title_full_unstemmed The role of ocean and atmospheric dynamics in the marine-based collapse of the last Eurasian Ice Sheet
title_short The role of ocean and atmospheric dynamics in the marine-based collapse of the last Eurasian Ice Sheet
title_sort role of ocean and atmospheric dynamics in the marine based collapse of the last eurasian ice sheet
url https://doi.org/10.1038/s43247-022-00447-0
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