| 摘要: |
| 自五十年代末以来，我国对南黄海124°E以西海区曾进行过不少的调查研究，对该海区的水文特征、水团结构和海流系统已有了基本的了解。但由于资料的限制，对124°E以东海区的情况了解尚少，所以有些问题，如黄海冷水团内部的温盐结构，黄海暖流以何种形式和以何路径进入南黄海等等，并不十分清楚。因此本文引用1983年11月中国科学院海洋研究所和美国伍兹霍尔海洋研究所在南黄海联合调查获得的Mark-III CTD 资料和浮标测流资料(站位见图1)，拟对南黄海秋末温、盐度垂直结构及其与流系之间的关系作一初步探讨。 |
| 关键词: 温盐度垂直结构 流系关系 |
| DOI： |
| 分类号: |
| 基金项目:中国科学院海洋研究所调查研究报告第1166号 |
|
| VERTICAL THERMOHALINE STRUCTURE AND ITS RELATION TO CURRENTS IN THE SOUTHERN YELLOW SEA IN LATE AUTUMN |
|
Ding Zongxin, Hu Dunxin, Xiong Qingcheng
|
|
Institute of Oceanology, Academia Sinica
|
| Abstract: |
| In the present paper, vertical thermohaline structure and its relation to currents in the Southern Yellow Sea are addressed, based on the temperature and salinity observations with Neil Brown Mark-III CTD and the current measurments from the bouys deployed in November, 1983. The thermohaline structure，which were firstly found in 1983，can be classified into these categories: (1) step structure caused by double diffusion, (2) double halocline structure., (3) temperature-inversion structure. Both the secondary halocline layer ?and temperature inversion layer were located in the Yellow Sea Cold Water at about the same depth, which suggests the existance of the Yellow Sea Warm Current.It appears that the Yellow Sea Warm Current, as a compensation current, flows into the central Southern Yellow Sea from west of Cheju Island in the bottom layer. |
| Key words: VERTICAL THERMOHALINE STRUCTURE CURRENTS |
