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	A review of research on the upwelling in the Taiwan Strait
	Hu, J. Y. ; Kawamura, H. ; Hong, H. S. ; Pan, W. R. ; Hong HS(洪华生)
	2003-09
关键词	WIND STRESS SEA CIRCULATION TOPOGRAPHY IMAGERY MODEL OCEAN
英文摘要	Research on upwelling in the Taiwan Strait, based on hydrographic observations and numerical modeling, has indicated that there are four upwelling regions in the Strait: along the Southwestern coast of the Taiwan Strait (SW-upwelling region), along the northwestern coast of the Taiwan Strait (NW-upwelling region), near the Taiwan Bank (TB-upwelling region), and around the Penghu Islands (PH-upwelling region). These upwellings are principally induced by the southwesterly monsoon and the ascending movement of the northward, near-bottom current along the uplifting bottom topography. The SW-upwelling and NW-upwelling occur during the southwesterly monsoon period in summer, and the TB-upwelling and PH-upwelling occur year-round with varying strength and scale.
语种	英语
内容类型	期刊论文
源URL	[http://dspace.xmu.edu.cn/handle/2288/60397]
专题	海洋环境－已发表论文
推荐引用方式 GB/T 7714	Hu, J. Y.,Kawamura, H.,Hong, H. S.,et al. A review of research on the upwelling in the Taiwan Strait[J],2003.
APA	Hu, J. Y.,Kawamura, H.,Hong, H. S.,Pan, W. R.,&洪华生.(2003).A review of research on the upwelling in the Taiwan Strait..
MLA	Hu, J. Y.,et al."A review of research on the upwelling in the Taiwan Strait".(2003).

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