南海深层环流与经向翻转环流的研究进展

发布时间：2018-05-27 10:43

本文选题：吕宋海峡“深水瀑布” + 南海深海环流　；参考：《中国科学:地球科学》2016年10期

【摘要】：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.
[Abstract]:Luzon Strait "Deepwater Falls" drives the deep cyclonic circulation in the South China Sea on the one hand, on the other hand, the invading deep waters of the North Pacific Ocean change and rise by mixing in the South China Sea. These two processes contribute greatly to the meridional reversal circulation in the South China Sea. At the same time, both the deep horizontal circulation and the meridional turnover circulation in the South China Sea are modulated by the complex topography in the South China Sea, and the spatial structure of the meridional turnover circulation in the South China Sea reflects to a certain extent the deep and middle circulation in the South China Sea. The connection of the upper circulation. In this paper, the deep circulation and meridional turnover circulation in the South China Sea are reviewed. The driving mechanism and topographic regulation of the deep-sea circulation in the South China Sea are summarized. The spatial structure and causes of the meridional reverse circulation in the South China Sea are summarized.
【作者单位】：中国科学院南海海洋研究所热带海洋环境国家重点实验室;中国科学院大学地球科学学院;中国科学院深海科学与工程研究所;
【基金】：中国科学院战略性先导专项项目(编号:XDB06020102);中国科学院三亚深海科学与工程研究所知识创新工程领域前沿项目(编号:SIDSSE-201205) 国家自然科学基金项目(批准号:41276024和91228202) 广东省科技计划项目(编号:2012A032100004)资助
【分类号】：P731.27

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