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Observational study of the circulation in the southern South China Sea

查看全文 作  者:Fang [1]Wendong;Guo [1]Zhongxin;Huang [1]Yuting 高影响力作者 机构地区:[1]Chinese Acad Sci, S China Sea Inst Oceanol, Guangzhou 510301, Peoples R China高影响力机构 出  处:《Chinese Science Bulletin》索引1998年第43卷第11期,共8页高影响力期刊 基  金:ThisworkwassupportedbytheNationalSpecialProject (GrantNo .85 92 7 0 5 0 1) 摘  要:CTD data from two oceanographic survey cruises, conducted by 'Shiyan No.3' R/V during two reversing monsoons, were employed to calculate and analyze the distributions of temperature, salinity and geopotential anomaly in the southern South China Sea (SSCS). Based on these distributions, the horizontal structures of the SSCS circulation are described systematically. Study results show that the SSCS circulation structure could be classified as a two-layer (the upper and the lower) pattern, and that the main circulation in the upper layer (0-400 m) is driven by the South China Sea monsoons and is opposite in direction to the reversal of the monsoons. The distributions of principal current systems and their features are presented. Two important local phenomena, local eddy and oceanic front, were observed. 关 键 词:SOUTHERN SOUTH China Sea CIRCULATION structure EDDY OCEANIC front.
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