FDM simulation of seismic-wave propagation for an aftershock of the 2009 Suruga bay earthquake: Effects of ocean-bottom topography and seawater layer

Takeshi Nakamura, Hiroshi Takenaka, Taro Okamoto, Yoshiyuki Kaneda

Research output: Contribution to journalArticle

29 Citations (Scopus)

Abstract

Feasibility studies on simulating seismic-wave propagation in media for a suboceanic earthquake, including both land and ocean-bottom topographies and a seawater layer, are scarce. Some of the conventional staggered-grid finite-difference method (FDM) simulations use a simplified structure model without a seawater layer and with a flat ocean-bottom topography. In this study, we apply our heterogeneity, oceanic layer, and topography scheme (HOT)-FDM and a 3D structure model including land and ocean-bottom topographies, a seawater layer, and a fluid-solid boundary condition to an aftershock (Mw 5.8) of the 2009 Suruga Bay earthquake.We attempt to reproduce observations at seismic stations near the coast and then simulate waveforms in the ocean-bottom stations. Our results show that a large difference between the cases with and without topographies can be seen in the coda part after the S wave in the simulated waveforms in terms of amplitudes and elongations. The synthetic waveforms in the model with topographies are in agreement with the observed waveforms. Our results also show that a significant difference in the amplification of the coda part between the cases with and without the seawater layer can be found at the ocean-bottom stations. This coda part is the S- and Rayleigh-wave propagation associated with the ocean and the underlying sediment layers. Our results show that a realistic model with topographies and a seawater layer is needed in FDM simulations in order to precisely reproduce observed waveforms or predict seismic motion for a suboceanic earthquake.

Original languageEnglish
Pages (from-to)2420-2435
Number of pages16
JournalBulletin of the Seismological Society of America
Volume102
Issue number6
DOIs
Publication statusPublished - Dec 2012
Externally publishedYes

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Earthquake effects
ocean bottom
Seismic waves
bottom topography
seismic waves
finite difference method
aftershock
Seawater
Finite difference method
seismic wave
Wave propagation
Topography
wave propagation
topography
earthquakes
seafloor
seawater
earthquake
waveforms
coda

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics

Cite this

FDM simulation of seismic-wave propagation for an aftershock of the 2009 Suruga bay earthquake : Effects of ocean-bottom topography and seawater layer. / Nakamura, Takeshi; Takenaka, Hiroshi; Okamoto, Taro; Kaneda, Yoshiyuki.

In: Bulletin of the Seismological Society of America, Vol. 102, No. 6, 12.2012, p. 2420-2435.

Research output: Contribution to journalArticle

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