| 对马暖流“东海段”的流路与流速 |
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| 引用本文： | 孙湘平.对马暖流“东海段”的流路与流速[J].海洋科学进展,1995(1). |
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| 作者姓名： | 孙湘平 |
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| 作者单位： | 国家海洋局第一海洋研究所 |
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| 摘 要： | 本文全面地分析了此段海流的流路与流速结构，首次提出研究海域近底层的环流示意图。指出在夏季，韩国南岸和日本九州北岸均存在着一支南下的逆流，九州西岸出现两种或多种形式的流路。对马暖流在源地流速很弱，流向不稳定，流路时隐时显不明显，只有离开源地后才逐渐显示出一支海流轮廓；强流区在朝鲜海峡附近。该海流可明显地划分为三段。流速夏强冬弱，夏季流幅宽约８０ｋｍ。
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| 关 键 词： | 对马暖流“东海段”，流路，流幅，流速结构 |
Path and Velocity of the Tsushima Warm Current in the East China Sea |
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| Sun Xiangping.Path and Velocity of the Tsushima Warm Current in the East China Sea[J].Advances in Marine Science,1995(1). |
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| Authors: | Sun Xiangping |
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| Abstract: | In this paper,the path and the velocity structure of the Tsushima Warm Current in the East China ho are analysed comprehensively. A schematic diagram of the near-bottom circulation in the studied area is presented for the first time. It shows that the southward countercurrents appear along both the souuthern coast of Korea and the northern coast of Kyushu Japan in summer,and that two or more typoes of the stream path occur off-shore of the western Kyushu. In its source area the velocity of the Tsushima Warm Current is very weak and its direction is uncertain. its path is unlear,sometime appering and sometime disapperaing. Only when the Tsushima Warm Current has left its source area does it reveal the contour of a current. The strong current occurs near the Korea Strait. The Tsushima Warm Current in the East China Sea can be divided obviously into three sectors. Its velocity is stronger in summer and weaker in winter. Its width is about 80km in summer. |
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| Keywords: | Tsushima Warm Current in the East China Sea stream path stream width velocity structure |
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