Seawater flux through Taiwan strait
Seawater flux through Taiwan strait
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DOI：
10.1007/bf02850748
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发表时间：
1991-09
影响因子：
--
通讯作者：
Fu Zilang;Huang Jianyu;Yu Guoming
中科院分区：
文献类型：
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作者：
Fu Zilang;Huang Jianyu;Yu Guoming
根据测得的海流资料得到台湾海峡两个或三个纬度断面上的冬、夏季流结构后，计算了通过这些断面的海水通量。夏季，台湾海峡中部和北部的海流通常向北流动，净通量为3.32×106m~3/S。冬季，高温、高盐度的黑潮和南中国海水分别以1.69×106m~3/S和0.59×106m~3/S的净通量从南侧进入台湾海峡，东中国海水以1.02×106m~3/S的净通量从北部进入台湾海峡，约0.40×106m~3/S的海水沿闽粤沿海进入中国南海；另有0.62×106m~3/S的海水与北部海域的黑潮水和南中国海水混合。冬季北上净通量为1.74×106m~3/S。
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 fluxs through the sections were calculated. In summer, the currents in the central and northern part of Taiwan Strait normally flow northward at a net flux of 3.32×106m3/s. In winter, the high temperature and salinity Kuroshio and South China Sea water enter Taiwan Strait from the southem section at 1.69×106m3/s and 0.59×106m3/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 areas. The net northward flux is 1.74×106m3/s in winter.