The Contributions of Winter Cloud Anomalies in 2011 to the Summer Sea-Ice Rebound in 2012 in the Antarctic
文献类型：期刊论文
| 作者 | 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
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| 刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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| 出版日期 | 2019-03-27 |
| 卷号 | 124期号:6页码:3435-3447 |
| 关键词 | cloud fraction cloud forcing sea ice Antarctic |
| ISSN号 | 2169-897X |
| DOI | 10.1029/2018JD029435 |
| 通讯作者 | Bi, Haibo(bhb@qdio.ac.cn) ; Huang, Haijun(hjhuang@qdio.ac.cn) |
| 英文摘要 | Unlike 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. |
| 资助项目 | National Natural Science Foundation of China[41406215] ; NSFC-Shandong Joint Fund for Marine Science Research Centers[U1606401] ; US NSF[PLR-1443444] |
| WOS研究方向 | Meteorology & Atmospheric Sciences |
| 语种 | 英语 |
| WOS记录号 | WOS:000464653500035 |
| 出版者 | AMER GEOPHYSICAL UNION |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/161125]  |
| 专题 | 海洋研究所_海洋地质与环境重点实验室 |
| 通讯作者 | Bi, Haibo; Huang, Haijun |
| 作者单位 | 1.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 |
| 推荐引用方式 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. |
入库方式： OAI收割
来源：海洋研究所
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