Progress on deep circulation and meridional overturning circulation in the South China Sea

被引：24
|
作者：
Wang DongXiao [1 ]
Xiao JinGen [1 ,2 ]
Shu YeQiang [1 ]
Xie Qiang [1 ,3 ]
Chen Ju [1 ]
Wang Qiang [1 ]
机构：
[1] Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou 510301, Guangdong, Peoples R China
[2] Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China
[3] Chinese Acad Sci, Inst Deep Sea Sci & Engn, Sanya 572000, Peoples R China
来源：
SCIENCE CHINA-EARTH SCIENCES | 2016年 / 59卷 / 09期
基金：
中国国家自然科学基金;
关键词：
Luzon overflow; SCS deep circulation; SCSMOC; Topography; LUZON STRAIT; DEPOSITIONAL CHARACTERISTICS; THERMOHALINE CIRCULATION; ABYSSAL CIRCULATION; NORTHWEST SUBBASIN; WORLD OCEAN; WATER; BASINS; SLOPE; MODEL;
D O I：
10.1007/s11430-016-5324-6
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
The deep overflow through the Luzon Strait drives the cyclonic deep circulation in the South China Sea (SCS). In the mean time, the intruding Pacific deep water transforms and upwells due to enhanced diapycnal mixing in the SCS. Both processes greatly contribute to the SCS meridional overturning circulation (SCSMOC). At the same time, both the deep circulation and meridional overturning circulation are modulated by rough topography in the SCS. Furthermore, the spatial structure of the SCSMOC infers a link between the upper-layer circulation and deep circulation in the SCS. This paper reviews recent advances in the SCS deep circulation and meridional overturning circulation, including the driving mechanism of the SCS deep circulation and its modulation by topography, as well as the spatial structure of the SCSMOC and its dynamical mechanism.
引用
收藏
页码：1827 / 1833
页数：7
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