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潮汐的搅拌作用,即潮混合,常常在中纬度陆架浅海中形成一种重要的水文现象——浅水陆架锋,亦称潮汐锋。黄海是一个半封闭的中纬度陆架浅海,水温的季节变化非常显著。黄海的潮能消耗又非常可观。据此,作者指出:夏季黄海的层化现象与潮混合有关;年复一年,黄海冷水团边界基本稳定,并且在冷水团边界附近海面总是存在着一些冷水分布,这类现象也是由潮混合形成的;由于近岸冷水的形成,在黄海冷水团边界附近海面还存在着浅水陆
Tidal mixing, tidal mixing, often forms an important hydrological phenomenon in the shallow shelf of the mid-latitude shelf - the shallow shelf front, also known as the tidal front. The Yellow Sea is a semi-enclosed, shallow-shelf, mid-latitude shelf where seasonal variations in water temperature are significant. The tidal energy consumption in the Yellow Sea is very impressive. Accordingly, the authors point out that stratification in the Yellow Sea in summer is related to tidal mixing. Year after year, the boundaries of the Yellow Sea cold water mass are basically stable, and there is always some cold water distribution on the sea surface near the boundary of the cold water mass. This phenomenon is also caused by tide Due to the formation of nearshore cold water, there is also a shallow water land near the boundary of the Yellow Sea cold water mass