IOCAS-IR  > 海洋地质与环境重点实验室
The Contributions of Winter Cloud Anomalies in 2011 to the Summer Sea-Ice Rebound in 2012 in the Antarctic
Wang, Yunhe1,4,5; Yuan, Xiaojun3; Bi, Haibo1,2,5; Liang, Yu1,4,5; Huang, Haijun1,2,4,5; Zhang, Zehua1,2,5; Liu, Yanxia1,2,5
2019-03-27
Source PublicationJOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
ISSN2169-897X
Volume124Issue:6Pages:3435-3447
Corresponding AuthorBi, Haibo(bhb@qdio.ac.cn) ; Huang, Haijun(hjhuang@qdio.ac.cn)
AbstractUnlike the rapid decline of Arctic sea ice in the warming climate, Antarctic sea-ice extent exhibits a modest positive trend in the period of near four decades. In recent years, the fluctuation in Antarctic sea ice has been strengthened, including a decrease toward the lowest sea-ice extent in February 2011 for the period of 1978-2016 and a strong rebound in the summer of 2012. The sea-ice recovery mainly occurs in the Weddell Sea, Bellingshausen Sea, Amundsen Sea, southern Ross Sea, and the eastern Somov Sea. This study offers a new mechanism for this summertime sea-ice rebound. We demonstrate that cloud-fraction anomalies in winter 2011 contributed to the positive Antarctic sea-ice anomaly in summer 2012. The results show that the negative cloud-fraction anomalies in winter 2011 related to the large-scale atmospheric circulation resulted in a substantial negative surface-radiation budget, which cooled the surface and promoted more sea-ice growth. The sea-ice growth anomalies due to the negative cloud forcing propagated by sea-ice motion vectors from September 2011 to January 2012. The distribution of the sea-ice anomalies corresponded well with the sea-ice concentration anomalies in February 2012 in the Weddell Sea and eastern Somov Sea. Thus, negative cloud-fraction anomalies in winter can play a vital role in the following summer sea-ice distribution.
Keywordcloud fraction cloud forcing sea ice Antarctic
DOI10.1029/2018JD029435
Indexed BySCI
Language英语
Funding ProjectNational Natural Science Foundation of China[41406215] ; NSFC-Shandong Joint Fund for Marine Science Research Centers[U1606401] ; US NSF[PLR-1443444]
WOS Research AreaMeteorology & Atmospheric Sciences
WOS SubjectMeteorology & Atmospheric Sciences
WOS IDWOS:000464653500035
PublisherAMER GEOPHYSICAL UNION
Citation statistics
Document Type期刊论文
Identifierhttp://ir.qdio.ac.cn/handle/337002/161126
Collection海洋地质与环境重点实验室
Corresponding AuthorBi, Haibo; Huang, Haijun
Affiliation1.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Geol & Environm, Qingdao, Shandong, Peoples R China
2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Shandong, Peoples R China
3.Columbia Univ, Lamont Doherty Earth Observ, New York, NY USA
4.Univ Chinese Acad Sci, Beijing, Peoples R China
5.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, Shandong, Peoples R China
First Author AffilicationInstitute of Oceanology, Chinese Academy of Sciences
Corresponding Author AffilicationInstitute of Oceanology, Chinese Academy of Sciences
Recommended Citation
GB/T 7714
Wang, Yunhe,Yuan, Xiaojun,Bi, Haibo,et al. The Contributions of Winter Cloud Anomalies in 2011 to the Summer Sea-Ice Rebound in 2012 in the Antarctic[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2019,124(6):3435-3447.
APA Wang, Yunhe.,Yuan, Xiaojun.,Bi, Haibo.,Liang, Yu.,Huang, Haijun.,...&Liu, Yanxia.(2019).The Contributions of Winter Cloud Anomalies in 2011 to the Summer Sea-Ice Rebound in 2012 in the Antarctic.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,124(6),3435-3447.
MLA Wang, Yunhe,et al."The Contributions of Winter Cloud Anomalies in 2011 to the Summer Sea-Ice Rebound in 2012 in the Antarctic".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 124.6(2019):3435-3447.
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