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学科主题: Oceanography
题名: Westward intensification in marginal seas
作者: Chen, GX ; Xue, HJ
通讯作者: chengengxin@scsio.ac.cn
关键词: Western boundary current ; South China Sea ; Gulf of Mexico ; Japan/East Sea ; Inflow ; Topography
刊名: OCEAN DYNAMICS
发表日期: 2014
卷: 64, 期:3, 页:337-345
收录类别: sci
部门归属: [Chen, Gengxin ; Xue, Huijie] Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou 510301, Guangdong, Peoples R China ; [Xue, Huijie] Univ Maine, Sch Marine Sci, Orono, ME USA
项目归属: LTO
资助者: Chinese Academy of Sciences [XDA11010103, SQ201302]; National Natural Science Foundation of China [41106027, 41206008, 91228202]; Guangzhou City Project for the Pearl River New Star in Science and Technology [2013J2200087]
摘要: An idealized model was used to examine why the strong western boundary current (WBC) is observed in the South China Sea (SCS) but not in the Gulf of Mexico (GOM) and Japan/East Sea (JES). Results suggested that the stronger WBC in the SCS is mainly attributed to the direct contribution of the inflow and the strong monsoon. Although the Gulf Stream transports a large amount of water into the GOM, the passage in the southeast corner guides the inflow out of the gulf and inhibits the inflow from intensifying the WBC. Meanwhile, the wind stress in the GOM is weakest among the three marginal seas. The meridional ocean ridge and the particular layout of the continental slope of JES prevent the whole basin from participating in the westward intensification. Besides, the throughflow has adverse effects on the formulation of WBC in JES. The variation of Coriolis parameter with latitude leads to the westward intensification in marginal seas. However, a strong WBC cannot be observed in the absence of reasonable collocation of wind, inflow, and topography.
原文出处: 查看原文
WOS记录号: WOS:000331980600003
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内容类型: 期刊论文
URI标识: http://ir.scsio.ac.cn/handle/344004/10571
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Chen, GX; Xue, HJ.Westward intensification in marginal seas,OCEAN DYNAMICS,2014,64(3):337-345
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