Global Drag-Coefficient Estimates From Scatterometer Wind and Wave Steepness
Liu, Guoqiang1,2; He, Yijun1; Shen, Hui1; Guo, Jie3
发表期刊IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING
ISSN0196-2892
2011-05-01
卷号49期号:5页码:1499-1503
关键词Air-sea Interaction Neural Networks (Nns) Remote Sensing
产权排序[Liu, Guoqiang; He, Yijun; Shen, Hui] Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China; [Liu, Guoqiang] Chinese Acad Sci, Key Lab Ocean Circulat & Waves, Grad Sch, Beijing 100039, Peoples R China; [Guo, Jie] Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China
通讯作者Liu, GQ, Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China.heyj@ms.qdio.ac.cn
作者部门信息集成与应用实验室 
英文摘要A neural-network model was developed to retrieve the wave steepness (delta), which was used to represent the sea state (particularly wave state), from the European Remote Sensing (ERS) scatterometer onboard ERS-1/2. Using the retrieved delta and scatterometer wind speed, we calculated and examined the drag coefficient (C-D) over the global ocean. The results show that C-D changes significantly when wave steepness is included in the calculation. Combining wave steepness and wind speed increases C-D by nearly 14% on average. That change is spatially variable, ranging from -18.76% for the tropical Eastern Pacific Ocean to 104% for the Southern Ocean.; A neural-network model was developed to retrieve the wave steepness (delta), which was used to represent the sea state (particularly wave state), from the European Remote Sensing (ERS) scatterometer onboard ERS-1/2. Using the retrieved delta and scatterometer wind speed, we calculated and examined the drag coefficient (C-D) over the global ocean. The results show that C-D changes significantly when wave steepness is included in the calculation. Combining wave steepness and wind speed increases C-D by nearly 14% on average. That change is spatially variable, ranging from -18.76% for the tropical Eastern Pacific Ocean to 104% for the Southern Ocean.
文章类型Article
资助机构National Natural Science Foundation of China [40906069, 40776094]; Shangdong 908 Project [SD-908-02-08]; Chinese Academy of Sciences [2006-1-15]; K. C. WONG Education Foundation
收录类别SCI
语种英语
关键词[WOS]SEA-SURFACE ROUGHNESS ; STRESS ; DEPENDENCE ; PARAMETERIZATION ; ALGORITHM ; SPEED ; MODEL
研究领域[WOS]Geochemistry & Geophysics ; Engineering ; Remote Sensing ; Imaging Science & Photographic Technology
WOS记录号WOS:000289906200001
引用统计
被引频次:8[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.yic.ac.cn/handle/133337/4913
专题中国科学院海岸带环境过程与生态修复重点实验室_海岸带信息集成与战略规划研究中心
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China
2.Chinese Acad Sci, Key Lab Ocean Circulat & Waves, Grad Sch, Beijing 100039, Peoples R China
3.Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China
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GB/T 7714
Liu, Guoqiang,He, Yijun,Shen, Hui,et al. Global Drag-Coefficient Estimates From Scatterometer Wind and Wave Steepness[J]. IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING,2011,49(5):1499-1503.
APA Liu, Guoqiang,He, Yijun,Shen, Hui,&Guo, Jie.(2011).Global Drag-Coefficient Estimates From Scatterometer Wind and Wave Steepness.IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING,49(5),1499-1503.
MLA Liu, Guoqiang,et al."Global Drag-Coefficient Estimates From Scatterometer Wind and Wave Steepness".IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING 49.5(2011):1499-1503.
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