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关于黄海的潮混合和浅水锋现象,中国和韩国的学者已有一些报道(赵保仁,1987a,b;赵保仁等,1992;Lie,H-J.,1989)。卫星图片和有关水文观测资料表明,夏季,黄海的浅水锋主要分布在苏北浅滩外侧、山东半岛的成山角—石岛近海、渤海海峡、西朝鲜湾和江华湾湾口附近及朝鲜半岛西南部近海。 为了深入了解黄海苏北浅滩外侧浅水锋的分布和水文结构,我们于1990年7月29日
As for the tide-mixing and shallow-water front phenomena in the Yellow Sea, some scholars in China and South Korea have reported (Zhao Baoren, 1987a, b; Zhao Baoren, etc., 1992; Lie, H-J., 1989). Satellite images and hydrographs show that in summer, the shallow-water front of the Yellow Sea mainly distributes on the outer side of the shallow north of the northern Jiangsu Peninsula, the Chengshanjiao-Shidao offshore, the Bohai Strait, the Gulf of West Korea and the Ganghwa Bay near the mouth of Shandong Peninsula and the offshore of southwestern part of the Korean Peninsula . In order to gain a better understanding of the distribution and hydrological structure of the shallow water front outside the shallow north of the North Yellow Sea,