黃海暖流源區(qū)附近水團特性及其季節(jié)變化
[Abstract]:According to the temperature and salt data released by (KODC), the simulated data of HYCOM model and the data of satellite altimeter, the method of water mass analysis is used in this paper. The distribution of water mass and its seasonal variation in the source area of the warm current are discussed in detail. The main conclusions are as follows: 1) in one year, there are mixed water of the warm current of the horse, the branch of Huang Hai of the warm water of the warm current of the horse, the mixed water of Huang Hai. East China Sea mixed water, the Yangtze River diluted water, Huang Hai cold water mass and Korea coastal water 7 kinds of water masses. There is a trend of westward intrusion of warm water in the southwest of Jeju Island and obvious seasonal variation. The warm current water in winter distributes all over the layer, and gradually weakens from spring to summer, and the depth of distribution decreases gradually. At the beginning of autumn, the invasion of the warm current in the bottom layer increased rapidly, even more than in the winter. 2) the source of Huang Hai branch of the warm water in summer was analyzed. The results show that: for the source area of the warm current, 50m is the Taiwan warm current water carried by the lateral branch of the Taiwan warm current continuation at a shallow level, and the Kuroshio water carried by the Kuroshio invasion of (Kuroshio Branch Current west of Kyushu, southwest of Kyushu by the Kuroshio (KBCW for short) at the depth of 50m; Taiwan warm water can not bypass Jeju Island into Huang Hai, and finally from the sea east of Jeju Island into the Strait of Malaysia, the summer warm water Huang Hai branch mainly originated from KBCW.
【學位授予單位】:中國科學院研究生院(海洋研究所)
【學位級別】:碩士
【學位授予年份】:2016
【分類號】:P731.16
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