摘要
对滦河口近海激流的形成进行了讨论,认为潮流的辐合和特殊的地形是激流形成的主要原因,而激流的大小则主要取决于无序位能的释放量。
On the formation of inshore storm current in the Luanhe River mouth area is discussed. The main formation causes of storm current are convergence of tidal current and special topography and the strength of storm current depends mainly on the released disordered potential energy.
出处
《科学技术与工程》
2002年第5期16-17,共2页
Science Technology and Engineering
基金
国家自然科学基金(49976009)