2008
DOI: 10.2208/proce1989.55.181
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Analysis of High Wave Disaster Mechanism Caused in Niigata and Toyama Prefectures on February 24, 2008

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“…The angular frequencies or the periods of continental edge waves can be estimated by the dispersion relationship proposed by Ursell 21) and Eckart 22) . In the case of bottom slope s <<1.0, they are expressed as 23) :…”
Section: (1) Tsunami Observed At Susaki Due To the 2011mentioning
confidence: 99%
“…The angular frequencies or the periods of continental edge waves can be estimated by the dispersion relationship proposed by Ursell 21) and Eckart 22) . In the case of bottom slope s <<1.0, they are expressed as 23) :…”
Section: (1) Tsunami Observed At Susaki Due To the 2011mentioning
confidence: 99%