南海深层水的来龙去脉  

Origin and development of the deep water in South China Sea

作　　者：王桂华 田纪伟 WANG Guihua;TIAN Jiwei(Department of Atmospheric and Oceanic Sciences&Institute of Atmospheric Sciences,Fudan University,Shanghai 200438,China;College of Oceanic and Atmospheric Sciences,Ocean University of China,Qingdao 266100,China)

机构地区：[1]复旦大学大气与海洋科学系/复旦大学大气科学研究院,上海200438 [2]中国海洋大学海洋与大气学院,青岛266100

出　　处：《科技导报》2020年第18期21-25,共5页Science & Technology Review

基　　金：国家自然科学基金重大研究计划项目(91428206,91628302);南方海洋科学与工程广东省实验室(珠海)深远海创新团队项目。

摘　　要：中国南海是一个半封闭、深海盆、多岛屿(海山)、多连通的边缘海,南海深层水十分活跃,更新时间快,具有典型的南海深层环流特征。综述了目前海洋学家对南海深层水的认知,厘清了南海深层水的来龙去脉,并阐述了南海深层环流的特色。The South China Sea(SCS)is a semi-enclosed and multi-connected marginal deep sea with a large number of islands(seamounts).The deep SCS circulation is very robust with active deep water renewed.This paper reviews the current understanding of the deep water in the SCS,focusing on its origin and development,as well as the unique features of the SCS deep circulation.

关 键 词：南海深层水 强混合 深层环流 

分 类 号：P731.2[天文地球—海洋科学]