Worldwide consequences of a mid-Holocene cooling in the Nordic Seas

The Earth's climate, marked by long-term shifts and punctuated events, shapes terrestrial and marine ecosystems. Despite the present interglacial period's warmth and stability compared to preceding glaciations, the Holocene has witnessed significant cooling events with worldwide consequenc...

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Main Authors: Telesiński, Maciej, Liu, Wei, Ren, Xianglin, Zajączkowski, Marek
Format: Article in Journal/Newspaper
Language:English
Published: California Digital Library (CDL) 2023
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00867/97910/107008.pdf
https://doi.org/10.31223/X5JQ0M
https://archimer.ifremer.fr/doc/00867/97910/
id ftarchimer:oai:archimer.ifremer.fr:97910
record_format openpolar
spelling ftarchimer:oai:archimer.ifremer.fr:97910 2024-01-14T10:05:45+01:00 Worldwide consequences of a mid-Holocene cooling in the Nordic Seas Telesiński, Maciej Liu, Wei Ren, Xianglin Zajączkowski, Marek 2023-11-10 application/pdf https://archimer.ifremer.fr/doc/00867/97910/107008.pdf https://doi.org/10.31223/X5JQ0M https://archimer.ifremer.fr/doc/00867/97910/ eng eng California Digital Library (CDL) https://archimer.ifremer.fr/doc/00867/97910/107008.pdf doi:10.31223/X5JQ0M https://archimer.ifremer.fr/doc/00867/97910/ info:eu-repo/semantics/openAccess restricted use EarthArXiv (California Digital Library (CDL)) In Press North Atlantic ocean circulation planktic foraminifera biomarkers abrupt changes East Asian monsoon text Article info:eu-repo/semantics/article 2023 ftarchimer https://doi.org/10.31223/X5JQ0M 2023-12-19T23:51:09Z The Earth's climate, marked by long-term shifts and punctuated events, shapes terrestrial and marine ecosystems. Despite the present interglacial period's warmth and stability compared to preceding glaciations, the Holocene has witnessed significant cooling events with worldwide consequences. Leveraging marine records from the Nordic Seas, we provide the first detailed account of a cooling event centered around 6.8 ka BP. Utilizing paleoceanographic proxies and advanced modelling, we unveil a distinct subsurface water cooling, associated with a stepwise increase in sea-ice cover in the eastern Fram Strait. Our findings emphasize the role of Greenland Sea deep convection onset and the subsequent westward shift in Atlantic Water flow, enabling sea-ice advection from the Barents Sea. The heightened sea-ice cover weakens Atlantic Water advection, perturbing overturning circulation in the eastern Nordic Seas. These perturbations propagate worldwide, affecting North Atlantic deep-water circulation, inducing widespread hemispheric cooling, shifting the Intertropical Convergence Zone southward, and weakening the East Asian monsoon. Incorporating rigorous modelling supports and augments proxy-based paleoreconstructions, underscoring sea-ice dynamics and ocean circulation's critical influence. This study highlights the potential for localized cooling events within ostensibly stable climatic intervals, underscoring the need to comprehend their mechanisms for precise climate predictions and informed policymaking toward a sustainable future. Article in Journal/Newspaper Barents Sea Fram Strait Greenland Greenland Sea Nordic Seas North Atlantic Deep Water North Atlantic Sea ice Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Barents Sea Greenland
institution Open Polar
collection Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer)
op_collection_id ftarchimer
language English
topic North Atlantic
ocean circulation
planktic foraminifera
biomarkers
abrupt changes
East Asian monsoon
spellingShingle North Atlantic
ocean circulation
planktic foraminifera
biomarkers
abrupt changes
East Asian monsoon
Telesiński, Maciej
Liu, Wei
Ren, Xianglin
Zajączkowski, Marek
Worldwide consequences of a mid-Holocene cooling in the Nordic Seas
topic_facet North Atlantic
ocean circulation
planktic foraminifera
biomarkers
abrupt changes
East Asian monsoon
description The Earth's climate, marked by long-term shifts and punctuated events, shapes terrestrial and marine ecosystems. Despite the present interglacial period's warmth and stability compared to preceding glaciations, the Holocene has witnessed significant cooling events with worldwide consequences. Leveraging marine records from the Nordic Seas, we provide the first detailed account of a cooling event centered around 6.8 ka BP. Utilizing paleoceanographic proxies and advanced modelling, we unveil a distinct subsurface water cooling, associated with a stepwise increase in sea-ice cover in the eastern Fram Strait. Our findings emphasize the role of Greenland Sea deep convection onset and the subsequent westward shift in Atlantic Water flow, enabling sea-ice advection from the Barents Sea. The heightened sea-ice cover weakens Atlantic Water advection, perturbing overturning circulation in the eastern Nordic Seas. These perturbations propagate worldwide, affecting North Atlantic deep-water circulation, inducing widespread hemispheric cooling, shifting the Intertropical Convergence Zone southward, and weakening the East Asian monsoon. Incorporating rigorous modelling supports and augments proxy-based paleoreconstructions, underscoring sea-ice dynamics and ocean circulation's critical influence. This study highlights the potential for localized cooling events within ostensibly stable climatic intervals, underscoring the need to comprehend their mechanisms for precise climate predictions and informed policymaking toward a sustainable future.
format Article in Journal/Newspaper
author Telesiński, Maciej
Liu, Wei
Ren, Xianglin
Zajączkowski, Marek
author_facet Telesiński, Maciej
Liu, Wei
Ren, Xianglin
Zajączkowski, Marek
author_sort Telesiński, Maciej
title Worldwide consequences of a mid-Holocene cooling in the Nordic Seas
title_short Worldwide consequences of a mid-Holocene cooling in the Nordic Seas
title_full Worldwide consequences of a mid-Holocene cooling in the Nordic Seas
title_fullStr Worldwide consequences of a mid-Holocene cooling in the Nordic Seas
title_full_unstemmed Worldwide consequences of a mid-Holocene cooling in the Nordic Seas
title_sort worldwide consequences of a mid-holocene cooling in the nordic seas
publisher California Digital Library (CDL)
publishDate 2023
url https://archimer.ifremer.fr/doc/00867/97910/107008.pdf
https://doi.org/10.31223/X5JQ0M
https://archimer.ifremer.fr/doc/00867/97910/
geographic Barents Sea
Greenland
geographic_facet Barents Sea
Greenland
genre Barents Sea
Fram Strait
Greenland
Greenland Sea
Nordic Seas
North Atlantic Deep Water
North Atlantic
Sea ice
genre_facet Barents Sea
Fram Strait
Greenland
Greenland Sea
Nordic Seas
North Atlantic Deep Water
North Atlantic
Sea ice
op_source EarthArXiv (California Digital Library (CDL)) In Press
op_relation https://archimer.ifremer.fr/doc/00867/97910/107008.pdf
doi:10.31223/X5JQ0M
https://archimer.ifremer.fr/doc/00867/97910/
op_rights info:eu-repo/semantics/openAccess
restricted use
op_doi https://doi.org/10.31223/X5JQ0M
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