scholarly journals SURFACE PATTERN OF THE SOUTH CHINA SEA WESTERN BOUNDARY CURRENT IN WINTER

2009 ◽  
pp. 99-107 ◽  
Author(s):  
ZHIGANG HE ◽  
DONGXIAO WANG
2012 ◽  
Vol 31 (5) ◽  
pp. 1-10 ◽  
Author(s):  
Guohong Fang ◽  
Gang Wang ◽  
Yue Fang ◽  
Wendong Fang

2019 ◽  
Vol 124 (10) ◽  
pp. 6983-6996
Author(s):  
Yangyang Lu ◽  
Zuozhu Wen ◽  
Dalin Shi ◽  
Wenfang Lin ◽  
Sophie Bonnet ◽  
...  

2016 ◽  
Vol 66 (6-7) ◽  
pp. 795-810 ◽  
Author(s):  
Qi Quan ◽  
Huijie Xue ◽  
Huiling Qin ◽  
Xuezhi Zeng ◽  
Shiqiu Peng

2017 ◽  
Vol 7 (1) ◽  
Author(s):  
Chun Zhou ◽  
Wei Zhao ◽  
Jiwei Tian ◽  
Xiaolong Zhao ◽  
Yuchao Zhu ◽  
...  

2020 ◽  
Vol 50 (10) ◽  
pp. 2953-2963
Author(s):  
Muping Zhou ◽  
Guihua Wang ◽  
Wenhu Liu ◽  
Changlin Chen

AbstractThe existence of a deep western boundary current (DWBC) in the South China Sea (SCS) was verified by direct observations from three current moorings deployed from September 2015 to September 2018. The average current speeds observed in the DWBC were around 1 cm s−1 along the northern boundary and 3 cm s−1 along the western boundary. The DWBC demonstrates significant intraseasonal variability in the 30–120-day-period band, which may come from the variability in the Luzon overflow or the eddies in the deep SCS forced by a stable Luzon overflow. In addition, observations found that this DWBC along the northern boundary can reverse its direction meridionally in the spring. Model results suggest that if the Luzon overflow decreases one-third of its typical transport, this current reversal can occur. This behavior can be explained through “relaxation” theory.


2013 ◽  
Vol 58 (11) ◽  
pp. 1205-1215 ◽  
Author(s):  
DongXiao Wang ◽  
QinYan Liu ◽  
Qiang Xie ◽  
ZhiGang He ◽  
Wei Zhuang ◽  
...  

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