Comparison of Inversion Method of Wide Angle Ocean Bottom Seismometer Profile: A Case Study of Profile OBS973-2 Across Liyue Bank in the South China Sea

2014 ◽  
Vol 57 (4) ◽  
pp. 607-618
Author(s):  
NIU Xiong-Wei ◽  
WEI Xiao-Dong ◽  
RUAN Ai-Guo ◽  
WU Zhen-Li
Keyword(s):  
South China Sea ◽  
South China ◽  
The South China Sea ◽  
Inversion Method ◽  
Ocean Bottom ◽  
Ocean Bottom Seismometer ◽  
Wide Angle ◽  
The South ◽  
China Sea

A Wide Angle Ocean Bottom Seismometer Experiment Across Liyue Bank, the Southern Margin of the South China Sea

2011 ◽  
Vol 54 (6) ◽  
pp. 1033-1044 ◽  
Author(s):  
Ai-Guo RUAN ◽  
Xiong-Wei NIU ◽  
Xue-Lin QIU ◽  
Jia-Biao LI ◽  
Zhen-Li WU ◽  
...  
Keyword(s):  
South China Sea ◽  
South China ◽  
The South China Sea ◽  
Ocean Bottom ◽  
Ocean Bottom Seismometer ◽  
Wide Angle ◽  
The South ◽  
China Sea ◽  
Southern Margin

Typhoon-Induced Microseisms around the South China Sea

2020 ◽  
Vol 91 (6) ◽  
pp. 3454-3468
Author(s):  
Seongjun Park ◽  
Tae-Kyung Hong
Keyword(s):  
South China Sea ◽  
South China ◽  
Bottom Topography ◽  
Pressure Change ◽  
Ocean Waves ◽  
The South China Sea ◽  
Ocean Bottom ◽  
The South ◽  
China Sea ◽  
Regional Factors

Abstract Microseisms in frequencies of 0.05–0.5 Hz are a presentation of solid earth response to the ocean waves that are developed by atmospheric pressure change. The South China Sea provides a natural laboratory with a closed ocean environment to examine the influence of regional factors on microseism development as well as the nature of microseisms. The microseisms induced by typhoons crossing over the South China Sea are investigated. Typhoons are typical transient sources of varying strengths and locations. Primary microseisms develop nearly stationary in the northeastern South China Sea for most typhoons, suggesting effective environment for excitation of primary microseisms. Typhoon-induced secondary microseisms develop around the typhoon paths with time delays varying up to one day. Typhoon-induced microseism amplitudes are proportional to the ocean-wave amplitudes in the source regions, decaying with distance. Ocean waves develop following the typhoons for days. The dominant frequency of typhoon-induced microseisms increases with time due to the influence of dispersive ocean waves. The microseisms are affected by regional factors including crustal structures, coastal geometry, ocean depth, and ocean-bottom topography.

Towards a 90% renewable energy future: A case study of an island in the South China Sea

2017 ◽  
Vol 142 ◽  
pp. 28-41 ◽  
Author(s):  
Bin Ye ◽  
Kai Zhang ◽  
JingJing Jiang ◽  
Lixin Miao ◽  
Ji Li
Keyword(s):  
Renewable Energy ◽  
South China Sea ◽  
South China ◽  
The South China Sea ◽  
The South ◽  
China Sea

Enhanced 3D prestack depth imaging of broadband data from the South China Sea: a case study

2016 ◽  
Vol 47 (3) ◽  
pp. 219-227 ◽  
Author(s):  
Hao Zhang ◽  
Jincheng Xu ◽  
Jinbo Li
Keyword(s):  
South China Sea ◽  
South China ◽  
The South China Sea ◽  
The South ◽  
Depth Imaging ◽  
China Sea

A case study of near-inertial oscillation in the South China Sea using mooring observations and satellite altimeter data

2011 ◽  
Vol 67 (6) ◽  
pp. 677-687 ◽  
Author(s):  
Lu Sun ◽  
Quanan Zheng ◽  
Dongxiao Wang ◽  
Jianyu Hu ◽  
Chang-Kuo Tai ◽  
...  
Keyword(s):  
South China Sea ◽  
South China ◽  
The South China Sea ◽  
Altimeter Data ◽  
Inertial Oscillation ◽  
The South ◽  
Satellite Altimeter ◽  
China Sea ◽  
Satellite Altimeter Data
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