Source inversion of W phase: speeding up seismic tsunami warning

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Source inversion of W phase: speeding up seismic tsunami warning

S U M M A R Y W phase is a long period phase arriving before S wave. It can be interpreted as superposition of the fundamental, first, second and third overtones of spheroidal modes or Rayleigh waves and has a group velocity from 4.5 to 9 km s−1 over a period range of 100–1000 s. The amplitude of long period waves better represents the tsunami potential of an earthquake. Because of the fast gro...

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Zacharie Duputel,1 Luis Rivera,2 Hiroo Kanamori1 and Gavin Hayes3 1Seismological Laboratory, California Institute of Technology, Pasadena, CA, USA. E-mail: [email protected] 2Institut de Physique du Globe de Strasbourg, IPGS UMR 7516, CNRS and Université de Strasbourg (EOST), France 3U.S. Geological Survey, National Earthquake Information Center (contracted by Synergetics, Inc.), Golden,...

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A STRIKING correlation between the occurrence of a short-period earthquake phase (T phase) traveling through the ocean with the speed of sound in sea water and the occurrence of tsunamis has been observed. The characteristics of the T phase are described and the data upon which the correlation is based are presented. Although further study is needed, the evidence at hand warrants the inclusion ...

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ژورنال

عنوان ژورنال: Geophysical Journal International

سال: 2008

ISSN: 0956-540X,1365-246X

DOI: 10.1111/j.1365-246x.2008.03887.x