Role of atmospheric factors in forcing Arctic sea ice variability

Yu Liang; Haibo Bi; Yunhe Wang; Zehua Zhang; Haijun Huang

doi:10.1007/s13131-020-1629-6

Volume 39 Issue 9

Sep. 2020

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Yu Liang, Haibo Bi, Yunhe Wang, Zehua Zhang, Haijun Huang. Role of atmospheric factors in forcing Arctic sea ice variability[J]. Acta Oceanologica Sinica, 2020, 39(9): 60-72. doi: 10.1007/s13131-020-1629-6

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Yu Liang, Haibo Bi, Yunhe Wang, Zehua Zhang, Haijun Huang. Role of atmospheric factors in forcing Arctic sea ice variability[J]. Acta Oceanologica Sinica, 2020, 39(9): 60-72. doi: 10.1007/s13131-020-1629-6

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Role of atmospheric factors in forcing Arctic sea ice variability

doi: 10.1007/s13131-020-1629-6

Yu Liang^{1, 2, 3, 4},
Haibo Bi^{1, 2, 3
,
,},
Yunhe Wang^{1, 2, 3, 4},
Zehua Zhang^{1, 2, 3},
Haijun Huang^{1, 2, 3, 4
,
,}

1.
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
2.
Laboratory for Marine Geology, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China
3.
Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China
4.
University of Chinese Academy of Sciences, Beijing 100049, China

Funds: The National Natural Science Foundation of China under contract Nos 41406215 and 41706194; a fund provided by the Qingdao National Laboratory for Marine Science and Technology; the National Natural Science Foundation of China (NSFC)-Shandong Joint Fund for Marine Science Research Centers under contract No. U1606401.

More Information

Corresponding author: E-mail: bhb@qdio.ac.cn; hjhuang@qdio.ac.cn
Received Date: 2019-06-28
Accepted Date: 2019-09-27

Available Online: 2020-12-28

Publish Date: 2020-09-25

Abstract

Abstract

The spatial structure of the Arctic sea ice concentration (SIC) variability and the connection to atmospheric as well as radiative forcing during winter and summer for the 1979–2017 period are investigated. The interannual variability with different spatial characteristics of SIC in summer and winter is extracted using the empirical orthogonal function (EOF) analysis. The present study confirms that the atmospheric circulation has a strong influence on the SIC through both dynamic and thermodynamic processes, as the heat flux anomalies in summer are radiatively forced while those in winter contain both radiative and “circulation-induced” components. Thus, atmospheric fluctuations have an explicit and extensive influence to the SIC through complex mechanisms during both seasons. Moreover, analysis of a variety of atmospheric variables indicates that the primary mechanism about specific regional SIC patterns in Arctic marginal seas are different with special characteristics.
- sea ice concentration,
- atmospheric circulation,
- surface radiation

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References(60)

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