Advances in research of the mid-deep South China Sea circulation

查看全文 作　　者：Dongxiao [1]WANG;Qiang [1]WANG;Shuqun [1]CAI;Xiaodong [1]SHANG;Shiqiu [1]PENG;Yeqiang [1]SHU;Jingen [2]XIAO;Xiaohui [3]XIE;Zhiwei [4]ZHANG;Zhiqiang [5]LIU;Jian [4]LAN;Dake [3]CHEN;Huijie [1]XUE;Guihua [6]WANG;Jianping [7]GAN;Xinong [8]XIE;Rui [9]ZHANG;Hui [8]CHEN;Qingxuan [4]YANG

机构地区：[1]State Key Laboratory of Tropical Oceanography,South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 510301,China;[2]School of Marine Science and Technology,Tianjin University,Tianjin 300072,China;[3]State Key Laboratory of Satellite Ocean Environment Dynamics,Second Institute of Oceanography,MNR,Hangzhou 310012,China;[4]Key Laboratory of Physical Oceanography,MOE,Ocean University of China,Qingdao 266003,China;[5]Department of Ocean Science and Engineering,Southern University of Science and Technology,Shenzhen 518055,China;[6]Institute of Atmospheric Sciences,Fudan University,Shanghai 200438,China;[7]Department of Mathematics and Division of Environment,Hong Kong University of Science and Technology,Hong Kong 999077,China;[8]College of Marine Science and Technology,China University of Geosciences,Wuhan 430074,China;[9]College of Oceanic and Earth,Xiamen University,Xiamen 361102,China

出　　处：《Science China Earth Sciences》索引2019年第62卷第12期,共13页

基　　金：supported by the National Key Research and Development Program of China (Grant No. 2018YFC1405701);the Key Research Program of Frontier Sciences, CAS (Grant No. QYZDJ-SSW-DQC022);the National Natural Science Foundation of China (Grant Nos. 41521005, 41730535, 41776036, 41676001 & 41776026);the National Key Research and Development Program (Grant No. 2017YFA0603201) 摘　　要：The South China Sea(SCS)is a large marginal sea connecting the Indian and Pacific oceans.Under the factors of monsoons,strait transport,and varied bathymetry,the SCS presents a three-layer structure and strong diapycnal mixing which is far greater than that in the open ocean.Theoretical analysis and observations reveal that internal tides,internal solitary waves,and strong winds are the sources of the strong mixing in the northern SCS.A major consequence of the strong mixing is an active mid-deep circulation system.This system promotes exchange of water between the SCS and adjacent oceans,and also regulates the upper layer of wind-driven circulation,making the 3 dimensional SCS circulation clearly different from that in other tropical and subtropical marginal seas.The mass transport capacity of the mid-deep circulation has a substantial impact on marine sedimentation,the biogeochemical cycle,and other processes in the SCS.This paper summarizes the recent advances in middeep sea circulation dynamics of the SCS,and discusses the opportunities and challenges in this area. 关键词：Mid-deep South China Sea CIRCULATION Diapycnal MIXING MULTI-SCALE processes interaction

相关文献

参考文献（122）
引证文献（12）
耦合文献（125）

参考文献(122)

引证文献(12)

耦合文献(125)

互联网出版许可证新出网证(渝)字10号全国400电话 - 免长途话费

Advances in research of the mid-deep South China Sea circulation

参考文献(122)

引证文献(12)

耦合文献(125)

用户提示