The linkage between autumn Barents-Kara sea ice and European cold winter extremes

While the Arctic's accelerated warming and sea ice decline have been associated with Eurasian cooling, debates persist between those attributing this to sea ice retreat and those to internal variability. Our study examines the association between autumn sea ice variability over the Barents-Kara...

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Published in:Frontiers in Climate
Main Authors: Di Cai, Gerrit Lohmann, Xianyao Chen, Monica Ionita
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2024
Subjects:
Online Access:https://doi.org/10.3389/fclim.2024.1345763
https://doaj.org/article/efb2226425a1463db2e48ec94c9ad3e7
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spelling ftdoajarticles:oai:doaj.org/article:efb2226425a1463db2e48ec94c9ad3e7 2024-09-15T18:09:51+00:00 The linkage between autumn Barents-Kara sea ice and European cold winter extremes Di Cai Gerrit Lohmann Xianyao Chen Monica Ionita 2024-02-01T00:00:00Z https://doi.org/10.3389/fclim.2024.1345763 https://doaj.org/article/efb2226425a1463db2e48ec94c9ad3e7 EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/fclim.2024.1345763/full https://doaj.org/toc/2624-9553 2624-9553 doi:10.3389/fclim.2024.1345763 https://doaj.org/article/efb2226425a1463db2e48ec94c9ad3e7 Frontiers in Climate, Vol 6 (2024) low sea ice Barents-Kara Seas European cold extremes Rossby wave atmospheric blocking Environmental sciences GE1-350 article 2024 ftdoajarticles https://doi.org/10.3389/fclim.2024.1345763 2024-08-05T17:49:56Z While the Arctic's accelerated warming and sea ice decline have been associated with Eurasian cooling, debates persist between those attributing this to sea ice retreat and those to internal variability. Our study examines the association between autumn sea ice variability over the Barents-Kara Seas and extreme cold winters in Europe. Using the observational data and composite analysis, we explore the interannual variability and the potential linkage between sea ice and atmospheric circulation patterns. It reveals a correlation with shifts toward a negative phase of North Atlantic Oscillation and more frequent episodes of the atmospheric blocking over Greenland and the North Atlantic. Furthermore, the negative phase of the North Atlantic Oscillation and enhanced blocking are closely related and mutually reinforcing, shaping the spatial distribution of cold anomalies over much of the European continent. Our results suggest a link between the unusual decrease in Barents-Kara Sea ice during autumn and the occurrence of intense European weather extremes in subsequent winter months, emphasizing the need for delving deeper into this relationship on monthly time scales to enhance our predictive capabilities for midlatitude extreme events. Article in Journal/Newspaper Greenland Kara Sea North Atlantic North Atlantic oscillation Sea ice Directory of Open Access Journals: DOAJ Articles Frontiers in Climate 6
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic low sea ice
Barents-Kara Seas
European cold extremes
Rossby wave
atmospheric blocking
Environmental sciences
GE1-350
spellingShingle low sea ice
Barents-Kara Seas
European cold extremes
Rossby wave
atmospheric blocking
Environmental sciences
GE1-350
Di Cai
Gerrit Lohmann
Xianyao Chen
Monica Ionita
The linkage between autumn Barents-Kara sea ice and European cold winter extremes
topic_facet low sea ice
Barents-Kara Seas
European cold extremes
Rossby wave
atmospheric blocking
Environmental sciences
GE1-350
description While the Arctic's accelerated warming and sea ice decline have been associated with Eurasian cooling, debates persist between those attributing this to sea ice retreat and those to internal variability. Our study examines the association between autumn sea ice variability over the Barents-Kara Seas and extreme cold winters in Europe. Using the observational data and composite analysis, we explore the interannual variability and the potential linkage between sea ice and atmospheric circulation patterns. It reveals a correlation with shifts toward a negative phase of North Atlantic Oscillation and more frequent episodes of the atmospheric blocking over Greenland and the North Atlantic. Furthermore, the negative phase of the North Atlantic Oscillation and enhanced blocking are closely related and mutually reinforcing, shaping the spatial distribution of cold anomalies over much of the European continent. Our results suggest a link between the unusual decrease in Barents-Kara Sea ice during autumn and the occurrence of intense European weather extremes in subsequent winter months, emphasizing the need for delving deeper into this relationship on monthly time scales to enhance our predictive capabilities for midlatitude extreme events.
format Article in Journal/Newspaper
author Di Cai
Gerrit Lohmann
Xianyao Chen
Monica Ionita
author_facet Di Cai
Gerrit Lohmann
Xianyao Chen
Monica Ionita
author_sort Di Cai
title The linkage between autumn Barents-Kara sea ice and European cold winter extremes
title_short The linkage between autumn Barents-Kara sea ice and European cold winter extremes
title_full The linkage between autumn Barents-Kara sea ice and European cold winter extremes
title_fullStr The linkage between autumn Barents-Kara sea ice and European cold winter extremes
title_full_unstemmed The linkage between autumn Barents-Kara sea ice and European cold winter extremes
title_sort linkage between autumn barents-kara sea ice and european cold winter extremes
publisher Frontiers Media S.A.
publishDate 2024
url https://doi.org/10.3389/fclim.2024.1345763
https://doaj.org/article/efb2226425a1463db2e48ec94c9ad3e7
genre Greenland
Kara Sea
North Atlantic
North Atlantic oscillation
Sea ice
genre_facet Greenland
Kara Sea
North Atlantic
North Atlantic oscillation
Sea ice
op_source Frontiers in Climate, Vol 6 (2024)
op_relation https://www.frontiersin.org/articles/10.3389/fclim.2024.1345763/full
https://doaj.org/toc/2624-9553
2624-9553
doi:10.3389/fclim.2024.1345763
https://doaj.org/article/efb2226425a1463db2e48ec94c9ad3e7
op_doi https://doi.org/10.3389/fclim.2024.1345763
container_title Frontiers in Climate
container_volume 6
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