Mesoscale eddies cases study at Xisha waters in the South China Sea in 2009/2010

2015 ◽  
Vol 120 (1) ◽  
pp. 517-532 ◽  
Author(s):  
Qiang Wang ◽  
Lili Zeng ◽  
Weidong Zhou ◽  
Qiang Xie ◽  
Shuqun Cai ◽  
...  
Keyword(s):  
South China Sea ◽  
South China ◽  
Mesoscale Eddies ◽  
The South China Sea ◽  
The South ◽  
China Sea ◽  
Cases Study

scholarly journals Impact of mesoscale eddies on the source funnel of sediment trap measurements in the South China Sea

2021 ◽  
pp. 102566
Author(s):  
Wentao Ma ◽  
Peng Xiu ◽  
Fei Chai ◽  
Lihua Ran ◽  
Martin G. Wiesner ◽  
...  
Keyword(s):  
South China Sea ◽  
South China ◽  
Sediment Trap ◽  
Mesoscale Eddies ◽  
The South China Sea ◽  
The South ◽  
China Sea

Impacts of mesoscale eddies in the South China Sea on biogeochemical cycles

2015 ◽  
Vol 65 (9-10) ◽  
pp. 1335-1352 ◽  
Author(s):  
Mingxian Guo ◽  
Fei Chai ◽  
Peng Xiu ◽  
Shiyu Li ◽  
Shivanesh Rao
Keyword(s):  
South China Sea ◽  
South China ◽  
Mesoscale Eddies ◽  
Biogeochemical Cycles ◽  
The South China Sea ◽  
The South ◽  
China Sea

scholarly journals Observed Near-Inertial Waves in the Northern South China Sea

2021 ◽  
Vol 13 (16) ◽  
pp. 3223
Author(s):  
Bing Yang ◽  
Po Hu ◽  
Yijun Hou
Keyword(s):  
Remote Sensing ◽  
South China Sea ◽  
South China ◽  
Mesoscale Eddies ◽  
Relative Vorticity ◽  
The South China Sea ◽  
Inertial Waves ◽  
The South ◽  
China Sea ◽  
Maximum Value

Characteristics of near-inertial waves (NIWs) induced by the tropical storm Noul in the South China Sea are analyzed based on in situ observations, remote sensing, and analysis data. Remote sensing sea level anomaly data suggests that the NIWs were influenced by a southwestward moving anticyclonic eddy. The NIWs had comparable spectral density with internal tides, with a horizontal velocity of 0.14–0.21 m/s. The near-inertial kinetic energy had a maximum value of 7.5 J/m3 and propagated downward with vertical group speed of 10 m/day. Downward propagation of near-inertial energy concentrated in smaller wavenumber bands overwhelmed upward propagation energy. The e-folding time of NIWs ranged from 4 to 11 days, and the larger e-folding time resulted from the mesoscale eddies with negative vorticity. Modified by background relative vorticity, the observed NIWs had both red-shifted and blue-shifted frequencies. The upward propagating NIWs had larger vertical phase speeds and wavelengths than downward propagating NIWs. There was energy transfer from the mesoscale field to NIWs with a maximum value of 8.5 × 10−9 m2 s−3 when total shear and relative vorticity of geostrophic currents were commensurate. Our results suggest that mesoscale eddies are a significant factor influencing the generation and propagation of NIWs in the South China Sea.

Influence of mesoscale eddies on primary production in the South China Sea during spring inter-monsoon period

2014 ◽  
Vol 33 (3) ◽  
pp. 118-128 ◽  
Author(s):  
Zifeng Hu ◽  
Yehui Tan ◽  
Xingyu Song ◽  
Linbin Zhou ◽  
Xiping Lian ◽  
...  
Keyword(s):  
South China Sea ◽  
Primary Production ◽  
South China ◽  
Mesoscale Eddies ◽  
The South China Sea ◽  
The South ◽  
Monsoon Period ◽  
China Sea
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