Interaction of the Kuroshio with the East and the South China Seas and Nonlinear Wave Dynamics in the South China Sea

2006 ◽  
Author(s):  
Pearn P. Niiler ◽  
Dong-Kyu Lee ◽  
Luca Centurioni
2016 ◽  
Vol 35 (9) ◽  
pp. 1-12 ◽  
Author(s):  
Tongya Liu ◽  
Jiexin Xu ◽  
Yinghui He ◽  
Haibin Lü ◽  
Yuan Yao ◽  
...  

2006 ◽  
Vol 21 (4) ◽  
pp. 377-385 ◽  
Author(s):  
Hui Jiang ◽  
Svante Björck ◽  
Lihua Ran ◽  
Yue Huang ◽  
Jiayin Li

2013 ◽  
Vol 26 (20) ◽  
pp. 8097-8110 ◽  
Author(s):  
Feng Nan ◽  
Huijie Xue ◽  
Fei Chai ◽  
Dongxiao Wang ◽  
Fei Yu ◽  
...  

Abstract Inferred from the satellite and in situ hydrographic data from the 1990s and 2000s, the Kuroshio intrusion into the South China Sea (SCS) had a weakening trend over the past two decades. Associated with the weakened Kuroshio intrusion, the Kuroshio loop and eddy activity southwest of Taiwan became weaker, whereas the water above the salinity minimum became less saline in the northern SCS. The sea surface height southwest of Taiwan increased at a slower rate compared to other regions of the SCS because of the weakened Kuroshio intrusion. Simulations using the Regional Ocean Modeling System (ROMS) Pacific model show that the strength of the Kuroshio intrusion into the SCS decreased from 1993 to 2010 with a negative trend, −0.24 sverdrups (Sv) yr−1 (1 Sv ≡ 106 m3 s−1), in the total Luzon Strait transport (LST). Although wind-induced Ekman transport through the Luzon Strait became weaker, the magnitude at 0.001 Sv yr−1 was too small to compensate for the negative trend of the LST. On the other hand, the piling up of the water induced by monsoon winds was an important mechanism for changing the pressure gradient across the Luzon Strait and eventually affecting the LST. The sea level gradient between the western Pacific and the SCS had a negative trend, −0.10 cm yr−1, corresponding to a negative trend in the geostrophic transport at −0.20 Sv yr−1. The Kuroshio transport east of Luzon Island also had a negative trend, which might also be linked to the weakening Kuroshio intrusion.


The Holocene ◽  
2013 ◽  
Vol 23 (6) ◽  
pp. 850-859 ◽  
Author(s):  
Jianguo Liu ◽  
Tiegang Li ◽  
Rong Xiang ◽  
Muhong Chen ◽  
Wen Yan ◽  
...  

Crustaceana ◽  
2015 ◽  
Vol 88 (12-14) ◽  
pp. 1439-1445 ◽  
Author(s):  
Li-Chan Xiao ◽  
Yong-Liang Wang ◽  
Zhong-Li Sha

A new species of Diogenes Dana, 1851, Diogenes bispinatus sp. nov., is described from the South China Sea. It is closely allied to Diogenes dorotheae Morgan & Forest, 1991 and D. patae Asakura & Godwin, 2006, but it morphologically differs from the latter in the length of the antennular peduncle, the number of spines on the ocular acicle, the shape of the antennal acicle and the number of spines, the shape of the palm of left cheliped and telson. A key to the species of Diogenes from China seas is provided.


2006 ◽  
Vol 62 (4) ◽  
pp. 559-575 ◽  
Author(s):  
Michael J. Caruso ◽  
Glen G. Gawarkiewicz ◽  
Robert C. Beardsley

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