Open AccessCharacterization of scattered seismic wavefields simulated in heterogeneous media with topography
Author(s) -
Kumagai Hiroyuki,
Saito Tatsuhiko,
O'Brien Gareth,
Yamashina Tadashi
Publication year - 2011
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2010jb007718
Subject(s) - scattering , isotropy , seismic wave , wavelength , computational physics , radiation , geology , geophysics , physics , optics
We performed numerical simulations of seismic waveforms with frequencies up to 10 Hz in heterogeneous media with topography to investigate the effects of topography and structural heterogeneity on seismic scattering. We used the simulated waveforms to test the source location method assuming isotropic radiation of S waves for long‐period events and tremor at volcanoes. The assumption of isotropic radiation has been shown previously to be valid in a high‐frequency band because of the path effect caused by the scattering of seismic waves. Our simulation results showed that distortion of the wavefields increased as the correlation distance of structural heterogeneity ( a ) decreased, as the frequency increased, and as the travel distance increased. Topography alone considerably distorted the wavefields. However, we found that strong scattering due to topography was suppressed if the correlation distance of structural heterogeneity was longer than the S wave wavelength. Isotropic radiation of S waves by scattering due to topography was not achieved in our simulations. Our results indicated that scattering due to structural heterogeneity becomes stronger than that due to topography at ka ≅ 1 and a = 50 m, where k is the wave number of the S waves. This suggests that strong short‐scale structural heterogeneity is required to achieve isotropic radiation of S waves. Although we could not reproduce isotropic radiation, our results support the validity of the assumption of isotropic radiation in the source location method.