Estimation of seismic wave velocity at seafloor surface and sound source localization based on transmitted wave observation with an ocean bottom seismometer offshore of Kamaishi, Japan
Abstract An in situ method of estimating the seismic wave velocity at the seafloor surface by observing the particle motion of a wave transmitted into the sediment is presented; this method uses a sound source whose location is known. Conversely, a sound source localization method using the obtained...
| Published in: | Japanese Journal of Applied Physics |
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| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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IOP Publishing
2016
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| Online Access: | http://dx.doi.org/10.7567/jjap.55.07kg01 http://stacks.iop.org/1347-4065/55/i=7S1/a=07KG01/pdf http://stacks.iop.org/1347-4065/55/i=7S1/a=07KG01?key=crossref.7bbd5d2f221a3037ba494537c21ad501 https://iopscience.iop.org/article/10.7567/JJAP.55.07KG01 https://iopscience.iop.org/article/10.7567/JJAP.55.07KG01/pdf |
| Summary: | Abstract An in situ method of estimating the seismic wave velocity at the seafloor surface by observing the particle motion of a wave transmitted into the sediment is presented; this method uses a sound source whose location is known. Conversely, a sound source localization method using the obtained seismic velocities and involving particle motion observation is also presented. Although this method is applicable only when the sound source exists within the critical incidence angle range, it is expected to contribute to the tracing of vocalizing baleen whales, which are unknown around Japanese waters. |
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