Marine seismic observation of internal solitary wave packets in the northeast South China Sea

Recently the novel seismic oceanography method has been reported to be an effective way to study the energetic internal solitary waves (ISWs) in the northern South China Sea. An optimized seismic‐oceanographic cruise was carried out to observe such near‐surface ISWs on Dongsha Plateau in July 2014....

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Bibliographic Details
Published in:Journal of geophysical research. Oceans 2015-12, Vol.120 (12), p.8487-8503
Main Authors: Tang, Qunshu, Hobbs, Richard, Wang, Dongxiao, Sun, Longtao, Zheng, Chan, Li, Jiabiao, Dong, Chongzhi
Format: Article
Language:English
Subjects:
China
Cruises
Data processing
Geophysics
Hydrographic data
internal solitary wave
Internal waves
Marine
Mathematical analysis
Mathematical models
Methods
Northeast
Oceanography
Satellites
Seismic activity
Seismic data processing
seismic oceanography
Seismic phenomena
Seismic surveys
Seismological data
Shallow water
Solitary waves
Solitons
South China Sea
Spatial discrimination
Spatial resolution
Surface properties
Target recognition
Vertical velocities
Wave packets
Wave propagation
Waveforms
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Summary:Recently the novel seismic oceanography method has been reported to be an effective way to study the energetic internal solitary waves (ISWs) in the northern South China Sea. An optimized seismic‐oceanographic cruise was carried out to observe such near‐surface ISWs on Dongsha Plateau in July 2014. Several soliton trains rather than single solitons were captured using the seismic technique. After seismic data processing, one prototypical rank‐ordered ISW packet on northeast side of Dongsha Island was clearly identified for further analysis. This included waveforms, propagation velocities, and vertical velocities for individual solitons. In this study, an improved scheme was applied to derive the transient phase velocities from the seismic data which is verified from independent satellite and hydrographic data. Analytical predictions from Korteweg‐de Vries equation fit better than the extended Korteweg‐de Vries equation ignoring background currents. Our results show that the seismic method can be successfully used to image targets in shallow water below 40 m and that seismic oceanography is a promising technique for studying near‐surface phenomena with high spatial resolution. Key Points: Captured soliton trains in the NE South China Sea using seismic reflection technique Extracting waveform and propagation parameters of solitons from seismic data Consistency with conventional satellite observation and analytical prediction
ISSN:2169-9275
2169-9291
DOI:10.1002/2015JC011362