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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Bibliographic Details
Published in:Environmental Research Letters
Main Authors: Wang, Yunhe, Yuan, Xiaojun, Cane, Mark A.
Format: Report
Language:English
Published: IOP Publishing Ltd 2022
Subjects:
Online Access:http://ir.qdio.ac.cn/handle/337002/178666
http://ir.qdio.ac.cn/handle/337002/178667
https://doi.org/10.1088/1748-9326/ac5272
id ftchinacasciocas:oai:ir.qdio.ac.cn:337002/178667
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spelling ftchinacasciocas:oai:ir.qdio.ac.cn:337002/178667 2023-05-15T13:24:03+02:00 Coupled mode of cloud, atmospheric circulation, and sea ice controlled by wave-3 pattern in Antarctic winter Wang, Yunhe Yuan, Xiaojun Cane, Mark A. 2022-04-01 http://ir.qdio.ac.cn/handle/337002/178666 http://ir.qdio.ac.cn/handle/337002/178667 https://doi.org/10.1088/1748-9326/ac5272 英语 eng IOP Publishing Ltd ENVIRONMENTAL RESEARCH LETTERS http://ir.qdio.ac.cn/handle/337002/178666 http://ir.qdio.ac.cn/handle/337002/178667 doi:10.1088/1748-9326/ac5272 cloud sea ice atmospheric circulation wave-3 Antarctic Environmental Sciences & Ecology Meteorology & Atmospheric Sciences Environmental Sciences 期刊论文 2022 ftchinacasciocas https://doi.org/10.1088/1748-9326/ac5272 2022-07-29T12:11:44Z 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. Report Amundsen Sea Antarc* Antarctic Sea ice Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR Antarctic Amundsen Sea Environmental Research Letters 17 4 044053
institution Open Polar
collection Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR
op_collection_id ftchinacasciocas
language English
topic cloud
sea ice
atmospheric circulation
wave-3
Antarctic
Environmental Sciences & Ecology
Meteorology & Atmospheric Sciences
Environmental Sciences
spellingShingle cloud
sea ice
atmospheric circulation
wave-3
Antarctic
Environmental Sciences & Ecology
Meteorology & Atmospheric Sciences
Environmental Sciences
Wang, Yunhe
Yuan, Xiaojun
Cane, Mark A.
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 Sciences & Ecology
Meteorology & Atmospheric Sciences
Environmental Sciences
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 Report
author Wang, Yunhe
Yuan, Xiaojun
Cane, Mark A.
author_facet Wang, Yunhe
Yuan, Xiaojun
Cane, Mark A.
author_sort Wang, Yunhe
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 Ltd
publishDate 2022
url http://ir.qdio.ac.cn/handle/337002/178666
http://ir.qdio.ac.cn/handle/337002/178667
https://doi.org/10.1088/1748-9326/ac5272
geographic Antarctic
Amundsen Sea
geographic_facet Antarctic
Amundsen Sea
genre Amundsen Sea
Antarc*
Antarctic
Sea ice
genre_facet Amundsen Sea
Antarc*
Antarctic
Sea ice
op_relation ENVIRONMENTAL RESEARCH LETTERS
http://ir.qdio.ac.cn/handle/337002/178666
http://ir.qdio.ac.cn/handle/337002/178667
doi:10.1088/1748-9326/ac5272
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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