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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