Coupled mode of cloud, atmospheric circulation, and sea ice controlled by wave-3 pattern in Antarctic winter

This study examines coupled relationships among clouds, atmospheric circulation, and sea ice in Antarctic winter. We find that the wave-3 pattern dominates the leading covariability mode among cloud, atmospheric circulation, and sea ice. Both horizontal transport and vertical motion contribute to cl...

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Published in:Environmental Research Letters
Main Authors: Yunhe Wang, Xiaojun Yuan, Mark A Cane
Format: Article in Journal/Newspaper
Language:English
Published: IOP Publishing 2022
Subjects:
Q
Online Access:https://doi.org/10.1088/1748-9326/ac5272
https://doaj.org/article/97ca9aff9cdd40128c012706b066c610
id ftdoajarticles:oai:doaj.org/article:97ca9aff9cdd40128c012706b066c610
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spelling ftdoajarticles:oai:doaj.org/article:97ca9aff9cdd40128c012706b066c610 2023-09-05T13:11:46+02:00 Coupled mode of cloud, atmospheric circulation, and sea ice controlled by wave-3 pattern in Antarctic winter Yunhe Wang Xiaojun Yuan Mark A Cane 2022-01-01T00:00:00Z https://doi.org/10.1088/1748-9326/ac5272 https://doaj.org/article/97ca9aff9cdd40128c012706b066c610 EN eng IOP Publishing https://doi.org/10.1088/1748-9326/ac5272 https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/ac5272 1748-9326 https://doaj.org/article/97ca9aff9cdd40128c012706b066c610 Environmental Research Letters, Vol 17, Iss 4, p 044053 (2022) cloud sea ice atmospheric circulation wave-3 Antarctic Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 article 2022 ftdoajarticles https://doi.org/10.1088/1748-9326/ac5272 2023-08-13T00:36:45Z This study examines coupled relationships among clouds, atmospheric circulation, and sea ice in Antarctic winter. We find that the wave-3 pattern dominates the leading covariability mode among cloud, atmospheric circulation, and sea ice. Both horizontal transport and vertical motion contribute to cloud formation, resulting in maximum cloud anomalies spatially between maximum meridional wind and pressure anomalies in the coupled system. The radiative effect of the clouds related to the wave-3 pattern can generate sea ice anomalies up to 12 cm thick in one month in the Amundsen Sea. It also strengthens the sea ice anomalies that are directly induced by low-level atmospheric circulation anomalies. In addition, the radiative forcing of the leading cloud mode in the lower troposphere is suppressed by the dynamic and thermodynamic effects of the circulation anomalies. These discoveries provide a better understanding of Antarctica’s interactive processes, and also offer physical evidence for climate model validations. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Sea ice Directory of Open Access Journals: DOAJ Articles Amundsen Sea Antarctic Environmental Research Letters 17 4 044053
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic cloud
sea ice
atmospheric circulation
wave-3
Antarctic
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
spellingShingle cloud
sea ice
atmospheric circulation
wave-3
Antarctic
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
Yunhe Wang
Xiaojun Yuan
Mark A Cane
Coupled mode of cloud, atmospheric circulation, and sea ice controlled by wave-3 pattern in Antarctic winter
topic_facet cloud
sea ice
atmospheric circulation
wave-3
Antarctic
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
description This study examines coupled relationships among clouds, atmospheric circulation, and sea ice in Antarctic winter. We find that the wave-3 pattern dominates the leading covariability mode among cloud, atmospheric circulation, and sea ice. Both horizontal transport and vertical motion contribute to cloud formation, resulting in maximum cloud anomalies spatially between maximum meridional wind and pressure anomalies in the coupled system. The radiative effect of the clouds related to the wave-3 pattern can generate sea ice anomalies up to 12 cm thick in one month in the Amundsen Sea. It also strengthens the sea ice anomalies that are directly induced by low-level atmospheric circulation anomalies. In addition, the radiative forcing of the leading cloud mode in the lower troposphere is suppressed by the dynamic and thermodynamic effects of the circulation anomalies. These discoveries provide a better understanding of Antarctica’s interactive processes, and also offer physical evidence for climate model validations.
format Article in Journal/Newspaper
author Yunhe Wang
Xiaojun Yuan
Mark A Cane
author_facet Yunhe Wang
Xiaojun Yuan
Mark A Cane
author_sort Yunhe Wang
title Coupled mode of cloud, atmospheric circulation, and sea ice controlled by wave-3 pattern in Antarctic winter
title_short Coupled mode of cloud, atmospheric circulation, and sea ice controlled by wave-3 pattern in Antarctic winter
title_full Coupled mode of cloud, atmospheric circulation, and sea ice controlled by wave-3 pattern in Antarctic winter
title_fullStr Coupled mode of cloud, atmospheric circulation, and sea ice controlled by wave-3 pattern in Antarctic winter
title_full_unstemmed Coupled mode of cloud, atmospheric circulation, and sea ice controlled by wave-3 pattern in Antarctic winter
title_sort coupled mode of cloud, atmospheric circulation, and sea ice controlled by wave-3 pattern in antarctic winter
publisher IOP Publishing
publishDate 2022
url https://doi.org/10.1088/1748-9326/ac5272
https://doaj.org/article/97ca9aff9cdd40128c012706b066c610
geographic Amundsen Sea
Antarctic
geographic_facet Amundsen Sea
Antarctic
genre Amundsen Sea
Antarc*
Antarctic
Sea ice
genre_facet Amundsen Sea
Antarc*
Antarctic
Sea ice
op_source Environmental Research Letters, Vol 17, Iss 4, p 044053 (2022)
op_relation https://doi.org/10.1088/1748-9326/ac5272
https://doaj.org/toc/1748-9326
doi:10.1088/1748-9326/ac5272
1748-9326
https://doaj.org/article/97ca9aff9cdd40128c012706b066c610
op_doi https://doi.org/10.1088/1748-9326/ac5272
container_title Environmental Research Letters
container_volume 17
container_issue 4
container_start_page 044053
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