毕海波^1,2,3, 杨清华⁴, 梁钰^1,2,4,3, 王云鹤^1,2,4,3, 张泽华^1,2,3, 付敏⁵, 黄海军^1,2,6,3
1.中国科学院海洋研究所海洋地质与环境重点实验室, 山东 青岛 266071;2.青岛海洋科学与技术国家实验室海洋地质过程与环境功能实验室, 山东 青岛 266237;3.中国科学院海洋研究所 大科学研究中心, 青岛 266071;4.中山大学, 广东 珠海 519000;5.国家海洋环境预报中心, 北京 100081;6.中国科学院大学, 北京 100049

摘要:
北极海冰对全球气候变化起重要的指示作用。除了海水冻结和融化过程以外，通过弗拉姆海峡（Fram Strait）的海冰输出也是影响北极海冰质量变化的重要动力机制。观测数据中的多源卫星遥感数据（尤其是辐射计观测数据）在获取大尺度连续观测方面具有独特的优势，在研究北极海冰输出面积通量变化方面有着广泛应用。本文总结了北极弗拉姆海峡、其他通道（S-FJL、FJL-SZ、加拿大群岛、Nares海峡通道）海冰输出面积或体积通量，着重介绍了弗拉姆海峡不同年龄海冰输出情况，并总结和分析了影响北极海冰输运的大尺度大气活动模态。最后，本文阐明北极海冰输出方面现有研究的不足之处以及未来的突破方向。
关键词:北极海冰输出卫星遥感大气活动北极海冰变化
DOI：10.11759/hykx20180819002
分类号:P237
基金项目:国家自然科学基金项目（41406215）；山东省-国家自然科学基金联合项目（U1606401）

A review of Arctic sea ice export
BI Hai-bo^1,2,3, YANG Qing-hua⁴, LIANG Yu^1,2,4,3, WANG Yun-he^1,2,4,3, ZHANG Ze-hua^1,2,3, FU Min⁵, HUANG Hai-jun^1,2,6,3
1.Key laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;2.Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China;3.Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China;4.Sun Yat-Sen University, Zhuhai 519000, China;5.National Marine Environmental Forecasting Center, State Oceanic Administration, Beijing 100081, China;6.University of Chinese Academy of Sciences, Beijing 100049, China
Abstract:
Arctic sea ice is an important indicator of global climate change. In addition to the freezing and melting processes of sea water, the sea ice output through the Fram Strait is also an important dynamic mechanism that affects the mass change of Arctic sea ice. Observation data, especially multi-source satellite remote sensing data (and radiometer data, in particular) have unique advantages in obtaining large-scale continuous observation, and these data are widely used in the study of the variation in the flux of the Arctic sea ice output area. In this paper, we summarize the sea ice output area or volume flux of other channels (S-FJL, FJL-SZ, Canada Islands Nares Channel), and highlight the sea ice output at different ages in the Fram Strait. We then summarize and analyze the large-scale active atmospheric modes that affect the transport of Arctic sea ice. Finally, we identify the deficiencies of existing research and the breakthrough represented by the investigation of future Arctic sea ice output.
Key words:Arctic sea ice exportsatellite remote sensingatmospheric circulationArctic sea ice variability





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