Modelled realistic daily variation in low winter sea-ice concentration over the Barents Sea amplifies Asian cold events
The boreal wintertime atmospheric responses, especially cold events over central Asia, to low sea-ice concentration (SIC) with and without realistic daily variation over the Barents Sea are explored with the Community Atmosphere Model version 4.0 (CAM4.0). The results show that the general atmospher...
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Norwegian Polar Institute
2022
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ftjpolarres:oai:journals.openacademia.net:article/7834 2023-05-15T14:50:27+02:00 Modelled realistic daily variation in low winter sea-ice concentration over the Barents Sea amplifies Asian cold events Duan, Shengni Jiang, Zhina Wen, Min 2022-11-01 application/pdf text/html application/epub+zip text/xml https://polarresearch.net/index.php/polar/article/view/7834 https://doi.org/10.33265/polar.v41.7834 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/7834/14963 https://polarresearch.net/index.php/polar/article/view/7834/14959 https://polarresearch.net/index.php/polar/article/view/7834/14960 https://polarresearch.net/index.php/polar/article/view/7834/14962 https://polarresearch.net/index.php/polar/article/view/7834 doi:10.33265/polar.v41.7834 Copyright (c) 2022 Shengni Duan, Zhina Jiang, Min Wen https://creativecommons.org/licenses/by-nc/4.0 CC-BY-NC Polar Research; Vol. 41 (2022) 1751-8369 Sea-ice loss extreme weather events Arctic Community Atmosphere Model info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2022 ftjpolarres https://doi.org/10.33265/polar.v41.7834 2023-01-04T23:49:34Z The boreal wintertime atmospheric responses, especially cold events over central Asia, to low sea-ice concentration (SIC) with and without realistic daily variation over the Barents Sea are explored with the Community Atmosphere Model version 4.0 (CAM4.0). The results show that the general atmospheric responses to approximately equal winter-mean Arctic sea-ice loss with a similar pattern but with climatological versus realistic daily variation are different. With the forcing of low SIC with climatological daily variation, Asian cold events become a little longer and stronger than in the control experiment; this mainly results from the enhancement of a 500-hPa Ural anticyclonic anomaly. However, the low SIC forcing that includes realistic daily variability greatly intensifies central Asian cold events and the cyclonic anomaly downstream of the Ural anticyclone. Further analysis reveals that Asian cold events are closely associated with Arctic deep warming at an intraseasonal time scale, which is also the strongest in the perturbed experiment forced by low SIC with realistic daily variation. This work provides a better understanding of the linkage between sea-ice variation over the Barents Sea and central Asian cold events, which may improve extreme weather prediction. It also implies that it is necessary to force air–sea coupling models and atmospheric models with realistic daily SIC in the study of the relationship between Arctic sea ice and mid-latitude cold events. Article in Journal/Newspaper Arctic Barents Sea Polar Research Sea ice Polar Research (E-Journal) Arctic Barents Sea Polar Research 41 |
institution |
Open Polar |
collection |
Polar Research (E-Journal) |
op_collection_id |
ftjpolarres |
language |
English |
topic |
Sea-ice loss extreme weather events Arctic Community Atmosphere Model |
spellingShingle |
Sea-ice loss extreme weather events Arctic Community Atmosphere Model Duan, Shengni Jiang, Zhina Wen, Min Modelled realistic daily variation in low winter sea-ice concentration over the Barents Sea amplifies Asian cold events |
topic_facet |
Sea-ice loss extreme weather events Arctic Community Atmosphere Model |
description |
The boreal wintertime atmospheric responses, especially cold events over central Asia, to low sea-ice concentration (SIC) with and without realistic daily variation over the Barents Sea are explored with the Community Atmosphere Model version 4.0 (CAM4.0). The results show that the general atmospheric responses to approximately equal winter-mean Arctic sea-ice loss with a similar pattern but with climatological versus realistic daily variation are different. With the forcing of low SIC with climatological daily variation, Asian cold events become a little longer and stronger than in the control experiment; this mainly results from the enhancement of a 500-hPa Ural anticyclonic anomaly. However, the low SIC forcing that includes realistic daily variability greatly intensifies central Asian cold events and the cyclonic anomaly downstream of the Ural anticyclone. Further analysis reveals that Asian cold events are closely associated with Arctic deep warming at an intraseasonal time scale, which is also the strongest in the perturbed experiment forced by low SIC with realistic daily variation. This work provides a better understanding of the linkage between sea-ice variation over the Barents Sea and central Asian cold events, which may improve extreme weather prediction. It also implies that it is necessary to force air–sea coupling models and atmospheric models with realistic daily SIC in the study of the relationship between Arctic sea ice and mid-latitude cold events. |
format |
Article in Journal/Newspaper |
author |
Duan, Shengni Jiang, Zhina Wen, Min |
author_facet |
Duan, Shengni Jiang, Zhina Wen, Min |
author_sort |
Duan, Shengni |
title |
Modelled realistic daily variation in low winter sea-ice concentration over the Barents Sea amplifies Asian cold events |
title_short |
Modelled realistic daily variation in low winter sea-ice concentration over the Barents Sea amplifies Asian cold events |
title_full |
Modelled realistic daily variation in low winter sea-ice concentration over the Barents Sea amplifies Asian cold events |
title_fullStr |
Modelled realistic daily variation in low winter sea-ice concentration over the Barents Sea amplifies Asian cold events |
title_full_unstemmed |
Modelled realistic daily variation in low winter sea-ice concentration over the Barents Sea amplifies Asian cold events |
title_sort |
modelled realistic daily variation in low winter sea-ice concentration over the barents sea amplifies asian cold events |
publisher |
Norwegian Polar Institute |
publishDate |
2022 |
url |
https://polarresearch.net/index.php/polar/article/view/7834 https://doi.org/10.33265/polar.v41.7834 |
geographic |
Arctic Barents Sea |
geographic_facet |
Arctic Barents Sea |
genre |
Arctic Barents Sea Polar Research Sea ice |
genre_facet |
Arctic Barents Sea Polar Research Sea ice |
op_source |
Polar Research; Vol. 41 (2022) 1751-8369 |
op_relation |
https://polarresearch.net/index.php/polar/article/view/7834/14963 https://polarresearch.net/index.php/polar/article/view/7834/14959 https://polarresearch.net/index.php/polar/article/view/7834/14960 https://polarresearch.net/index.php/polar/article/view/7834/14962 https://polarresearch.net/index.php/polar/article/view/7834 doi:10.33265/polar.v41.7834 |
op_rights |
Copyright (c) 2022 Shengni Duan, Zhina Jiang, Min Wen https://creativecommons.org/licenses/by-nc/4.0 |
op_rightsnorm |
CC-BY-NC |
op_doi |
https://doi.org/10.33265/polar.v41.7834 |
container_title |
Polar Research |
container_volume |
41 |
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1766321472741048320 |