| On the Taiwan Warm Current Water |
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| 作者姓名： | 翁学传 王从敏 |
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| 作者单位： | Institute of Oceanology，Academia Sinica，Institute of Oceanology，Academia Sinica |
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| 摘 要： | Using our data from special observation in the source area of the Taiwan Warm Current from 19S2 to 1985) and historical data, the authors conducted studies to clarify the temperature and salinity characteristics, variability, and origin of the Taiwan Warm Current Water, and its influence on the expanding direction of the Changjiang Diluted Water.The main results of these studies are briefly given below. (1) The Taiwan Warm Current Water can be divided into two parts:the Surface Water of the Taiwan Warm Current and the Deep Water of the Taiwan Warm Current; the former is formed due to the mixing of the Kuroshio Surface Water flowing northward along the east coast of Taiwan with the Taiwan Strait Water; the latter completed originates from Kuroshio Subsurface Water to the east of Taiwan. It is characterized by lower temperature and higher salinity in summer and the characteristics of temperature and salinity are more stable. The maximum seasonal variational range and maximum secular variational range of t
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On the Taiwan Warm Current Water |
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| Weng Xuechuan and Wang Congmin.On the Taiwan Warm Current Water[J].Periodical of Ocean University of China,1989(Z1). |
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| Authors: | Weng Xuechuan and Wang Congmin |
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| Abstract: | |
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| Keywords: | water mass the Taiwan Warm Current Water |
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