Insolation triggered abrupt cooling at the end of interglacials and implication for the future ...

<!--!introduction!--> Various paleoclimate records show that the end of interglacials of the late Pleistocene was marked by abrupt cooling events. Strong abrupt cooling occurring when climate was still in a warm interglacial condition is puzzling. Our transient climate simulations for the elev...

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Main Authors: Yin, Qiuzhen, Wu, Zhipeng, Liang, Ming-Qiang, Berger, Andre
Format: Article in Journal/Newspaper
Language:unknown
Published: GFZ German Research Centre for Geosciences 2023
Subjects:
Online Access:https://dx.doi.org/10.57757/iugg23-0980
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016509
id ftdatacite:10.57757/iugg23-0980
record_format openpolar
spelling ftdatacite:10.57757/iugg23-0980 2023-06-11T04:13:47+02:00 Insolation triggered abrupt cooling at the end of interglacials and implication for the future ... Yin, Qiuzhen Wu, Zhipeng Liang, Ming-Qiang Berger, Andre 2023 https://dx.doi.org/10.57757/iugg23-0980 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016509 unknown GFZ German Research Centre for Geosciences Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Oral ConferencePaper Article 2023 ftdatacite https://doi.org/10.57757/iugg23-0980 2023-05-02T11:08:17Z <!--!introduction!--> Various paleoclimate records show that the end of interglacials of the late Pleistocene was marked by abrupt cooling events. Strong abrupt cooling occurring when climate was still in a warm interglacial condition is puzzling. Our transient climate simulations for the eleven interglacial (sub)stages of the past 800,000 years show that, when summer insolation in the Northern Hemisphere (NH) high latitudes decreases to a critical value (a threshold), it triggers a strong, abrupt weakening of the Atlantic meridional overturning circulation and consequently an abrupt cooling in the NH. The mechanism involves sea ice-ocean feedbacks in the Northern Nordic Sea and the Labrador Sea (Yin et al., 2021, doi: 10.1126/science.abg1737). The insolation-induced abrupt cooling is accompanied by abrupt changes in precipitation, vegetation from low to high latitudes and in particular by abrupt snow accumulation in polar regions. The timing of the simulated abrupt events at the end of interglacials ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Article in Journal/Newspaper Labrador Sea Nordic Sea Sea ice DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description <!--!introduction!--> Various paleoclimate records show that the end of interglacials of the late Pleistocene was marked by abrupt cooling events. Strong abrupt cooling occurring when climate was still in a warm interglacial condition is puzzling. Our transient climate simulations for the eleven interglacial (sub)stages of the past 800,000 years show that, when summer insolation in the Northern Hemisphere (NH) high latitudes decreases to a critical value (a threshold), it triggers a strong, abrupt weakening of the Atlantic meridional overturning circulation and consequently an abrupt cooling in the NH. The mechanism involves sea ice-ocean feedbacks in the Northern Nordic Sea and the Labrador Sea (Yin et al., 2021, doi: 10.1126/science.abg1737). The insolation-induced abrupt cooling is accompanied by abrupt changes in precipitation, vegetation from low to high latitudes and in particular by abrupt snow accumulation in polar regions. The timing of the simulated abrupt events at the end of interglacials ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ...
format Article in Journal/Newspaper
author Yin, Qiuzhen
Wu, Zhipeng
Liang, Ming-Qiang
Berger, Andre
spellingShingle Yin, Qiuzhen
Wu, Zhipeng
Liang, Ming-Qiang
Berger, Andre
Insolation triggered abrupt cooling at the end of interglacials and implication for the future ...
author_facet Yin, Qiuzhen
Wu, Zhipeng
Liang, Ming-Qiang
Berger, Andre
author_sort Yin, Qiuzhen
title Insolation triggered abrupt cooling at the end of interglacials and implication for the future ...
title_short Insolation triggered abrupt cooling at the end of interglacials and implication for the future ...
title_full Insolation triggered abrupt cooling at the end of interglacials and implication for the future ...
title_fullStr Insolation triggered abrupt cooling at the end of interglacials and implication for the future ...
title_full_unstemmed Insolation triggered abrupt cooling at the end of interglacials and implication for the future ...
title_sort insolation triggered abrupt cooling at the end of interglacials and implication for the future ...
publisher GFZ German Research Centre for Geosciences
publishDate 2023
url https://dx.doi.org/10.57757/iugg23-0980
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016509
genre Labrador Sea
Nordic Sea
Sea ice
genre_facet Labrador Sea
Nordic Sea
Sea ice
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.57757/iugg23-0980
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