Japan Geoscience Union Meeting 2014

Presentation information

Oral

Symbol S (Solid Earth Sciences) » S-SS Seismology

[S-SS27_29AM1] Seismic wave propagation: Theory and Application

Tue. Apr 29, 2014 9:00 AM - 10:45 AM 411 (4F)

Convener:*Tatsuhiko Saito(National Research Institute for Earth Science and Disaster Prevention), Hisashi Nakahara(Solid Earth Physics Laboratory, Department of Geophysics, Graduate School of Science, Tohoku University), Jun Matsushima(School of Engineering, The University of Tokyo), Kiwamu Nishida(Earthquake Research Institute, University of Tokyo), Kazuya Shiraishi(JGI, Inc.), Chair:Yohei Yukutake(Hot Springs Research Institute of Kanagawa Prefecture), Kazuya Shiraishi(JGI, Inc.)

10:00 AM - 10:15 AM

[SSS27-05] The roles of dispersion and nonlinear effects in the 2001 Tohoku-Oki earthquake tsunami

*Tatsuhiko SAITO1, Daisuke INAZU1 (1.National Research Institute for Earth Science and Disaster Prevention)

Keywords:tsunami, dispersion, nonlinear wave, the 2011 Tohoku-Oki earthquake

The present study aims to reveal the roles of the dispersion and the nonlinear effects in the 2011 Tohoku-Oki earthquake tsunami. Tsunami simulations were conducted based on the nonlinear dispersive equations with a high-resolution source model. The result successfully reproduced the waveforms recorded in both near shore and deep sea. The calculated inundation area showed a good coincidence with the actual inundation at the Sendai Plain, the widest inundation area during this event. Conducting sets of simulations using different equations, we obtained the followings insights. Although the dispersion was neglected in most studies, the maximum-amplitude distribution was significantly overestimated in the deep sea if the dispersion was not included. The waveform observed at the station in which the largest tsunami height (> 2 m) recorded among deep-ocean stations also verified the necessity of the dispersion. It is well known that the nonlinear effects play an important role for the tsunami inside bays and harbors. Additionally, the nonlinear effects needed be considered for the accurate modeling of the later waves even at the offshore stations. In particular, including nonlinear terms rather than including the inundation was more important for the precise modeling of the waves reflected from the coast.