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Yang Kun, Shi Ping, Wang Dongxiao, You Xiaobao, Li Rongfeng. Numerical study about the mesoscale multi-eddy system in the northern South China Sea in winter[J]. Haiyang Xuebao, 2000, 22(1): 27-34.
Citation:
Yang Kun, Shi Ping, Wang Dongxiao, You Xiaobao, Li Rongfeng. Numerical study about the mesoscale multi-eddy system in the northern South China Sea in winter[J]. Haiyang Xuebao, 2000, 22(1): 27-34.
Yang Kun, Shi Ping, Wang Dongxiao, You Xiaobao, Li Rongfeng. Numerical study about the mesoscale multi-eddy system in the northern South China Sea in winter[J]. Haiyang Xuebao, 2000, 22(1): 27-34.
Citation:
Yang Kun, Shi Ping, Wang Dongxiao, You Xiaobao, Li Rongfeng. Numerical study about the mesoscale multi-eddy system in the northern South China Sea in winter[J]. Haiyang Xuebao, 2000, 22(1): 27-34.
A numerical model is successfully used to simulate and analyze the multi-eddy system in the northern South China Sea in winter.The evoluation of multi-eddy system is affected by various factors:the baroclinic adjustment is the crucia[ one.Both the lateral boundary forcing and the realistic wind stress are important to the forming and maintaining of multi-eddy system.In order to illustrate the mechanism of evolution of the multi-eddy system,the vertical structures are analyzed in detail.The result of numerical modelling displays the dynamic evolution proeess of the multi-eddy system in tho northern South China Sea:an anticyclone appears with Kuroshio's intrusion in winter near the Bashi Strait; then it is advected by the large-scale circulation and goes forward to the west and the south,gradually splitting into an eddy array.With eneegy exchange with the background field,the anticyclone army disappears at the western boundary.It is indicated that the intrusion into the South China Sea of Kuroshio mainly appears in form of eddy.
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