论文部分内容阅读
吕宋海峡“深水瀑布”一方面驱动了南海深层气旋式环流,另一方面入侵的北太平洋深层水在南海内区通过混合变性并上升.这两个过程极大地贡献了南海经向翻转环流.同时无论是南海深层水平环流,还是经向翻转环流,均受到南海内区复杂地形的调制,而南海经向翻转环流的空间结构又在一定程度上体现了南海深层环流与中、上层环流的联系.本文回顾了近年来南海深层环流与经向翻转环流的研究,总结了南海深海环流的驱动机制及其地形的调控、南海经向翻转环流的空间结构及其成因.
On the one hand, the Luzon Strait, driven by the deep-sea cyclonic circulation in the South China Sea, on the one hand, and the deep in the North Pacific invaded through denaturalization and rising in the South China Sea by mixing, both of which contributed greatly to the warp inversion of the South China Sea Meanwhile, both the horizontal circulation in the deep sea of the South China Sea and the overturning circulation in the meridional direction are modulated by the complicated terrain in the South China Sea. The spatial structure of the overturning circulation in the South China Sea reflects to some extent the deep circulation in the South China Sea and the middle and upper circulation This paper reviews the recent research on the deep and meridional circulation in the South China Sea, summarizes the driving mechanism of the South China Sea deep-sea circulation and the regulation of its terrain, the spatial structure and its causes of the inversion of the meridional circulation in the South China Sea.