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Wang Huiqun,Yuan Yaochu. 1997. Calculation of currents in Taiwan Strait during summer Ⅰ. Three-dimensional diagnostic calculation. Acta Oceanologica Sinica, (4):441－457
Calculation of currents in Taiwan Strait during summer Ⅰ. Three-dimensional diagnostic calculation
Calculation of currents in Taiwan Strait during summer Ⅰ. Three-dimensional diagnostic calculation
Received:June 25, 1996  Revised:October 28, 1996
DOI：
Key words:Taiwan Strait  current  three-dimension diagnostic
中文关键词:  Taiwan Strait  current  three-dimension diagnostic
基金项目:
Author NameAffiliation
Wang Huiqun Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China 
Yuan Yaochu Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China 
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Abstract:
      A three-dimensional nonlinear model in a coordinate is set up and used to calculate the currents in the Taiwan Strait (TS) with hydrographic data collected during summer of 1984 end 1988.It is shown that there is a persistent northward current with the volume transport(VT) of 0.83×106 m3/s through the TS during summer.Among them, the VT through the eastern and western part of the southern boundary of the strait is 0.58×106 m3/s and 0.25×106 m3/s, respectively.The velocity is the strongest in the eastern part of the TS and comes sernnd in the western part of the TS.The upwelling generally occurs near Fujian coast.On the current features in the TS during summer, the density current is primary and the wind-driven current is of secondary importance.
中文摘要:
      A three-dimensional nonlinear model in a coordinate is set up and used to calculate the currents in the Taiwan Strait (TS) with hydrographic data collected during summer of 1984 end 1988.It is shown that there is a persistent northward current with the volume transport(VT) of 0.83×106 m3/s through the TS during summer.Among them, the VT through the eastern and western part of the southern boundary of the strait is 0.58×106 m3/s and 0.25×106 m3/s, respectively.The velocity is the strongest in the eastern part of the TS and comes sernnd in the western part of the TS.The upwelling generally occurs near Fujian coast.On the current features in the TS during summer, the density current is primary and the wind-driven current is of secondary importance.
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