摘要
After the winter and summer current structures on two or three latitudinal sections in Taiwan Strait were obtained from the measured current data, the seawater flux through the sections were cal -culated. In summer, the currents in the central and northern part of Taiwan Strait normally flow northward at a net flux of 3.32×l06m3 /s. In winter, the high temperature and salinity Kuroshio and South China Sea water enter Taiwan Strait from the southern section at 1.69× 106m3/s and 0.59×10 m3/s respectively, while the East China Sea water enters Taiwan Strait from the northern section at 1.02×106m3/s. About 0.40×106m3/s of the seawater enters the South China Sea along the coast of Fujian and Guangdong; the other 0.62×106m3/s of the seawater is mixed with the Kuroshio water and the South China Sea water in the northern sea area . The net northward flux is 1.74×106m3/s in winter.
After the winter and summer current structures on two or three latitudinal sections in Taiwan Strait were obtained from the measured current data, the seawater flux through the sections were cal -culated. In summer, the currents in the central and northern part of Taiwan Strait normally flow northward at a net flux of 3.32×l06m3 /s. In winter, the high temperature and salinity Kuroshio and South China Sea water enter Taiwan Strait from the southern section at 1.69× 106m3/s and 0.59×10 m3/s respectively, while the East China Sea water enters Taiwan Strait from the northern section at 1.02×106m3/s. About 0.40×106m3/s of the seawater enters the South China Sea along the coast of Fujian and Guangdong; the other 0.62×106m3/s of the seawater is mixed with the Kuroshio water and the South China Sea water in the northern sea area . The net northward flux is 1.74×106m3/s in winter.
