In this paper, the air-sea planetary boundary is divided into three layers. With the aid of geostrophic momentum approximation, wind and current profiles, surface wind, surface wind stress and Ekman pumpinii in the atmosphere as well as in the ocean affected by the atmospheric baroclini-city, stratification and nonlinear effects are investigated systematically for an ocean of infinite depth. Meanwhile, the characteristics of the air-sea interaction is analyzed.
机构:
Chinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R ChinaChinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R China
Li, Qilong
Cheng, Xueling
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Chinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R China
Univ Chinese Acad Sci, Coll Earth Sci, Beijing, Peoples R ChinaChinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R China
Cheng, Xueling
Zeng, Xiaodong
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Chinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R ChinaChinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R China
Zeng, Xiaodong
Zhou, Guangqing
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Chinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R ChinaChinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R China
Zhou, Guangqing
Huang, Jian
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机构:
China Meteorol Adm, Inst Trop & Marine Meteorol, Guangzhou, Peoples R ChinaChinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R China
Huang, Jian
Wu, Lin
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Chinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R ChinaChinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R China
Wu, Lin
Zeng, Qingcun
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Chinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R ChinaChinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R China