Arctic Sea Ice Area Export Through the Fram Strait Estimated From Satellite-Based Data: 1988-2012 | |
Bi, Haibo1; Sun, Ke2; Zhou, Xuan3; Huang, Haijun1; Xu, Xiuli2 | |
刊名 | IEEE JOURNAL OF SELECTED TOPICS IN APPLIED EARTH OBSERVATIONS AND REMOTE SENSING
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2016-07-01 | |
卷号 | 9期号:7页码:3144-3157 |
关键词 | Fram Strait remote sensing sea ice area flux |
英文摘要 | By combing ice motion and concentration fields, we obtain the estimates of ice area flux passing the Fram Strait over a 25-year period (1988-2012). Mean monthly area flux exhibits a prominent cycle with the peak in March (78 x 10(3) km(2)/month) and the trough in August (5 x 10(3) km(2)/month). Mean net annual ice area flux (644.1 x 10(3) km(2) km(2)) is primarily/slightly attributable to winter (October-May)/summer (June-September) outflow of 598.7 x 10(3) km(2) (or 93.0%)/45.4 x 10(3) km(2) (or 7%). However, these quantities need to be considered with great prudence since comparisons with preceding studies indicate distinct difference may exist between calculated Fram Strait sea ice outflow based on varied ice motion datasets. In particular, major bias emerged during winter rather than summer. Trends are also affected due to this bias. Despite the clear disparity in magnitude, we found a good agreement with preceding estimates in terms of temporal variability. The linkage between ice area flux via the Fram Strait and various atmospheric circulation indices, such as the Arctic Oscillation (AO), the North Atlantic Oscillation (NAO), a west-east dipole anomaly pattern (DA), as well as a seesaw structure between Beaufort and Barents Sea (BBO), was examined. Results show that atmospheric circulation patterns linked to the DA and BBO possess a relatively stronger influence on Fram Strait ice export over the 25-year period. By contrast, the AO- and NAO-related atmospheric circulation pattern exhibit weaker connections with ice outflow through the strait. In addition, correlation analysis further justify the robust connection with a cross-strait surface level pressure gradient index. Depending on months, it is suggested that a manifold of aforementioned atmospheric indices may jointly or alone impose a significant influence on sea ice export through the Fram Strait. |
收录类别 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000384905500027 |
内容类型 | 期刊论文 |
版本 | 出版稿 |
源URL | [http://ir.qdio.ac.cn/handle/337002/136187] ![]() |
专题 | 海洋研究所_海洋地质与环境重点实验室 |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266061, Peoples R China 2.Lab Marine Geol & Environm, Qingdao 266061, Peoples R China 3.Chinese Acad Sci, Inst Elect, Beijing 100190, Peoples R China |
推荐引用方式 GB/T 7714 | Bi, Haibo,Sun, Ke,Zhou, Xuan,et al. Arctic Sea Ice Area Export Through the Fram Strait Estimated From Satellite-Based Data: 1988-2012[J]. IEEE JOURNAL OF SELECTED TOPICS IN APPLIED EARTH OBSERVATIONS AND REMOTE SENSING,2016,9(7):3144-3157. |
APA | Bi, Haibo,Sun, Ke,Zhou, Xuan,Huang, Haijun,&Xu, Xiuli.(2016).Arctic Sea Ice Area Export Through the Fram Strait Estimated From Satellite-Based Data: 1988-2012.IEEE JOURNAL OF SELECTED TOPICS IN APPLIED EARTH OBSERVATIONS AND REMOTE SENSING,9(7),3144-3157. |
MLA | Bi, Haibo,et al."Arctic Sea Ice Area Export Through the Fram Strait Estimated From Satellite-Based Data: 1988-2012".IEEE JOURNAL OF SELECTED TOPICS IN APPLIED EARTH OBSERVATIONS AND REMOTE SENSING 9.7(2016):3144-3157. |
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