| SOME PROBLEMS ON THE FLOW IN THE SOUTH OF THE EAST CHINA SEA |
| |
| 作者姓名： | 郭炳火 林葵 宋万先 |
| |
| 作者单位： | First Institute of Oceanography，State Oceanic Administration，Qingdao，First Institute of Oceanography，State Oceanic Administration，Qingdao，First Institute of Oceanography，State Oceanic Administration，Qingdao |
| |
| 摘 要： | Based on the observational current meter data from two mooring systems located between Chilung and the Pengjiayu Island from July 1980 to July 1981, and other oceanographic observational data in the south of the East China Sea, some problems on the flow of seawater in this area in summer are analysed in this paper. It is considered that a possible passage where the subsurface water of the Kuroshio flows into continental shelf area of the East China Sea is the lower layer of the region between Chilung and the point of 122°30′ E, 25°40′N. After passing through this passage, it flows roughly towards northeast along about 100 m isobath. The "Taiwan Warm Current" coming from the Taiwan Strait only passes through the upper layer of this area. The influence of the Taiwan Island on the flow and the eddies in this area are also discussed.
|
| 收稿时间： | 1984/12/14 0:00:00 |
| 修稿时间： | 1985/2/10 0:00:00 |
SOME PROBLEMS ON THE FLOW IN THE SOUTH OF THE EAST CHINA SEA |
| |
| GUO BINGHUO,LIN KUI and SONG WANXIAN.SOME PROBLEMS ON THE FLOW IN THE SOUTH OF THE EAST CHINA SEA[J].Acta Oceanologica Sinica,1986,5(1):22-31. |
| |
| Authors: | GUO BINGHUO LIN KUI and SONG WANXIAN |
| |
| Institution: | First Institute of Oceanography, State Oceanic Administration, Qingdao |
| |
| Abstract: | Based on the observational current meter data from two mooring systems located between Chilung and the Pengjiayu Island from July 1980 to July 1981,and other oceanographic observational data in the south of the East China Sea,some problems on the flow of seawater in this area in summer are analysed in this paper.It is considered that a possible passage where the subsurface water of the Kuroshio flows into continental shelf area of the East China Sea is the lower layer of the region between Chilung and the point of 122°30' E,25°40'N.After passing through this passage,it flows roughly towards northeast along about 100 m isobath.The "Taiwan Warm Current" coming from the Taiwan Strait only passes through the upper layer of this area.The influence of the Taiwan Island on the flow and the eddies in this area are also discussed. |
| |
| Keywords: | |
| 本文献已被 CNKI 等数据库收录！ |
| 点击此处可从《海洋学报(英文版)》浏览原始摘要信息 |
| 点击此处可从《海洋学报(英文版)》下载免费的PDF全文 |
