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YUAN Yao-chu, LIU Yong-gang, LOU Ru-yun, SU Ji-lan, WANG Kang-shan. Calculation of circulation in the South China Sea during the summer of 2000 by the modified inverse method[J]. Haiyang Xuebao, 2004, 26(1): 1-13.
Citation: YUAN Yao-chu, LIU Yong-gang, LOU Ru-yun, SU Ji-lan, WANG Kang-shan. Calculation of circulation in the South China Sea during the summer of 2000 by the modified inverse method[J]. Haiyang Xuebao, 2004, 26(1): 1-13.

Calculation of circulation in the South China Sea during the summer of 2000 by the modified inverse method

  • Received Date: 2003-05-04
  • Rev Recd Date: 2003-07-10
  • On the basis of hydrographic data obtained in August 2000 cruise,the circulation in the South China Sea (SCS)is computed by using the modified inverse method in combination with SSH data from TOPEX/ER S-2 Analysis.The following results have been obtained.(1)The central and southw estern SCSs are dominated mainly by anticyclonic circulation systems.They are mainly as follows.1)There is strong anticyclonic eddy southeast of Vietnam(W1).Its horizontal scale is about 300 km,and it extends vertically from the surface to the 1 000 m more than.It is very strong with a Vmax of about 79 cm/s;2)there are a warm eddy W2 and the anticyclonic circulation system W3 west off the Philippines.In the next place,there is a stronger cyclonic eddy C1 between the anticy clonic eddies W1 and W2,and it is also strong.A southward flow exists between the eddies W1 and C1.The eddies W1 and C1 compose a quasi-dipole.(2)A strong coastal jet is present at the western boundary west of an anticy clonic eddy W1,and the jet flows northward and separates from the coast of Vietnam at about 12°N to the northeast.
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