| 摘要: |
| 本文根据作者于1984年2月—1985年9月在台湾海峡、 闽东渔场、台湾北部海域和浙江外海海域投放“人工水母”的结果,对台湾暖流区的底层流进行了分析。结果表明:台湾暖流区的底层流比较稳定,各季的流向皆为北向流。其中,除闽、浙外海春季为北偏西向流外,其余皆为东北向流或正北向流。本文还得出,在台湾海峡中部和北部海域,冬季和春季的底层流与夏季一样是东北向流,而不是传统所认为的西南向流。 |
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| THE OBSERVATION OF BOTTOM CURRENT IN THE AREA OF TAIWAN WARM CURRENT |
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| Abstract: |
| In order to explain the origin of Taiwan Warm Current， an observation of the bottom current in the area of Taiwan Warm Current was carried out by using the "sea-bed drif-ter" during the time from Feb., 1984 to Sep., 1985. The results show that the bottom current of Taiwan Warm Current is relatively stable, and its directions are all towards the north the year round (east by north or west by north). In the areas of the mid part and northern part of the Taiwan Strait, the bottom current in spring and winter just like that in the summer, is rather northeastward, than southwestward as regarded traditionally. |
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