Westward intensification in marginal seas
Chen, GX; Xue, HJ; chengengxin@scsio.ac.cn
2014
发表期刊OCEAN DYNAMICS
ISSN1616-7341
卷号64期号:3页码:337-345
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.
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
关键词Western Boundary Current South China Sea Gulf Of Mexico Japan/east Sea Inflow Topography
学科领域Oceanography
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] ; 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] ; 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] ; 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]
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收录类别sci
资助项目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] ; 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] ; 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] ; 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]
WOS记录号WOS:000331980600003
引用统计
文献类型期刊论文
条目标识符http://ir.scsio.ac.cn/handle/344004/10571
专题热带海洋环境国家重点实验室(LTO)
通讯作者chengengxin@scsio.ac.cn
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GB/T 7714
Chen, GX,Xue, HJ,chengengxin@scsio.ac.cn. Westward intensification in marginal seas[J]. OCEAN DYNAMICS,2014,64(3):337-345.
APA Chen, GX,Xue, HJ,&chengengxin@scsio.ac.cn.(2014).Westward intensification in marginal seas.OCEAN DYNAMICS,64(3),337-345.
MLA Chen, GX,et al."Westward intensification in marginal seas".OCEAN DYNAMICS 64.3(2014):337-345.
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