| THE KUROSHIO (ON THE PN SECTION) IN THE EAST CHINA SEA DURING 1972-1983 |
| |
| 作者姓名： | 浦泳修 许小云 |
| |
| 作者单位： | The Second Institute of Oceanography，State Oceanic Adiministration Hangzhou，The Second Institute of Oceanography，State Oceanic Adiministration Hangzhou |
| |
| 摘 要： | The current elements of the Kuroshio in the East China Sea are analysed and discussed using the temperature-salinity and GEK data of the PN section obtained during 1972-1983. The calculations have proved (i) that the 12-year's mean volume transport of the Kuroshio at PN in the 0-800 m layer is about 20×106m3/s; (ii) that the mean volume transport has seasonal variations, i. e. slightly stronger in spring and summer than in the other seasons; and (iii) that the period of high-volume transport thereof corresponds to the appearance of a meander of the Kuroshio south of Japan. It is also discovered that this Kuroshio meander usually appears after a sharp increase in such volume transport. Finally, the differences of the Kuroshio volume transport between the PN, E and Suao-Yonakuni-jima sections are discussed.
|
| 收稿时间： | 4/6/1985 12:00:00 AM |
| 修稿时间： | 1985/10/4 0:00:00 |
THE KUROSHIO (ON THE PN SECTION) IN THE EAST CHINA SEA DURING 1972-1983 |
| |
| PU YONGXIU and XU XlAOYUN.THE KUROSHIO (ON THE PN SECTION) IN THE EAST CHINA SEA DURING 1972-1983[J].Acta Oceanologica Sinica,1987,6(1):37-45. |
| |
| Authors: | PU YONGXIU and XU XlAOYUN |
| |
| Institution: | The Second Institute of Oceanography, State Oceanic Adiministration Hangzhou |
| |
| Abstract: | The current elements of the Kuroshio in the East China Sea are analysed and discussed using the temperature-salinity and GEK data of the PN section obtained during 1972-1983.The calculations have proved (ⅰ) that the 12-year's mean volume transport of the Kuroshio at PN in the 0-800 m layer is about 20×106m3/s; (ⅱ) that the mean volume transport has seasonal variations, i.e.slightly stronger in spring and summer than in the other seasons; and (ⅲ) that the period of high-volume transport thereof corresponds to the appearance of a meander of the Kuroshio south of Japan.It is also discovered that this Kuroshio meander usually appears after a sharp increase in such volume transport.Finally, the differences of the Kuroshio volume transport between the PN, E and Suao-Yonakuni-jima sections are 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 |
