| 摘要: |
| 在南黄海的东南部，有一支较强的高温、高盐水入侵，这一水体通常称为黄海暖流，也有人称之为南黄海高盐水。从环流和水团的结构来看，这一水体来源于济州岛东南的对马暖流，我们则称之为南黄海暖流水。本文试图从水团分析角度研究这一水体的温、盐度分布基本特征。
南黄海暖流水自对马暖流分出后，沿西北方向侵入南黄海，对黄海、渤海、东海的海洋环境有着重大的影响。也更因其高温特征，携带大量热量，对我国沿海地区和朝鲜半岛的气候也有一定的影响。所以，它很早就引起了国内外海洋学界的重视。我国曾于六十年代初期对黄海暖流作过研究，但研究海区仅局限于124°E以西海域。
本文引用的海洋观测资料包括中国和南朝鲜在1976-1979年间在南黄海及其东部邻近海区的(双月)调查资料(共计141个测站)。研究海区向东扩至128°E 。 |
| 关键词: 南黄海暖流 温、盐度分布 |
| 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1064号 |
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| CHARACTERISTICS OF TEMPERATURE AND SALINITY OF THE SOUTHERN YELLOW SEA WARM CURRENT WATER |
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Lan Shufang, Gu Chuancheng, Fu Bingzhao
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Institute of Oceanology, Academia Sinica
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| Abstract: |
| In the south-east of the Southern Yellow Sea., there is often a strong intrusion water with higher temperature and salinity originated from Tsushima Current. It is named at the present the Southern Yellow Sea Warm Current Water. Using the data from National Oceanographic Bureau of China and Fisheries Research and Development Agency of the Republic of Korea for years 1976-1979, the authors obtained the average December temperature-salinity of the body of the Southern Yellow Sea Warm Current Water, its seasonal changes, and its year by year variance. The results of its T-S Diagram analysis are presented. |
| Key words: TEMPERATURE AND SALINITY THE SOUTHERN YELLOW SEA WARM CURRENT WATER |
