TY - JOUR
T1 - An Optimum 2D Seismic-Wavefield Reconstruction in Densely and Nonuniformly Distributed Stations
T2 - The Metropolitan Seismic Observation Network in Japan
AU - Shiina, Takahiro
AU - Maeda, Takuto
AU - Kano, Masayuki
AU - Kato, Aitaro
AU - Hirata, Naoshi
N1 - Funding Information:
for the Promotion of Science (JSPS) Grants-in-Aid for Scientific Research (KAKENHI) program (Grant Number JP19K04006). The authors used the Earthquake Information Center (EIC) computer system of the Earthquake Research Institute, the University of Tokyo, for numerical simulations. Most figures in this article were made using the Generic Mapping Tools (GMT) software of Wessel and Smith (1998).
Funding Information:
Constructive and careful reviews provided by three anonymous reviewers greatly improved the article. This study was supported by Japan Science and Technology Agency (JST) Core Research for Evolutional Science and Technology (CREST) program (Grant Number JPMJCR1763). T. M. was also supported by Japan Society
Publisher Copyright:
© 2021 Seismological Society of America. All rights reserved.
PY - 2021
Y1 - 2021
N2 - We propose an optimization method for applying the seismic-wave gradiometry (SWG) method to a dense seismic station network consisting of nonuniformly distributed seismographs. As a nonuniformly distributed station array, we consider the station layout of the Metropolitan Seismic Observation Network (MeSO-net) operated in and around the Tokyo metropolitan area, Japan. In this study, thereby, we numerically investigate optimum shapes of weighting functions, which control the spatial weights of individual stations when estimating waveforms at any grid points in the SWG method, to reconstruct seismic wavefields propagating in the MeSO-net. The functions with isotropic spatial weights are found to be appropriate for wavefield reconstructions with seismic waves incoming from practically all directions, even for nonuniformly distributed stations. The reproducibility of the wavefields is greatly improved by changing the shapes of the spatial weights reflecting density of the stations. Further plausible wavefield reconstructions are made by considering the propagation directions of the seismic waves. In these cases, if theweight of a contribution for a wavefield reconstruction is larger at far stations with a direction perpendicular to the wave propagation direction, then the reproducibility of the waveforms is significantly increased. In addition, the spatial gradients of the amplitudes are well reproduced by the optimized SWG method even though the optimization only focused on the amplitudes. Therefore, our proposed optimization scheme can be used to accurately estimate seismic wavefields in a nonuniformly distributed station array. Actually, the weighting functions optimized in this study succeeded to reconstruct the seismic wavefield of a shallow crustal earthquake that occurred around the Tokyo metropolitan area, based on the observed seismograms obtained by the MeSO-net.
AB - We propose an optimization method for applying the seismic-wave gradiometry (SWG) method to a dense seismic station network consisting of nonuniformly distributed seismographs. As a nonuniformly distributed station array, we consider the station layout of the Metropolitan Seismic Observation Network (MeSO-net) operated in and around the Tokyo metropolitan area, Japan. In this study, thereby, we numerically investigate optimum shapes of weighting functions, which control the spatial weights of individual stations when estimating waveforms at any grid points in the SWG method, to reconstruct seismic wavefields propagating in the MeSO-net. The functions with isotropic spatial weights are found to be appropriate for wavefield reconstructions with seismic waves incoming from practically all directions, even for nonuniformly distributed stations. The reproducibility of the wavefields is greatly improved by changing the shapes of the spatial weights reflecting density of the stations. Further plausible wavefield reconstructions are made by considering the propagation directions of the seismic waves. In these cases, if theweight of a contribution for a wavefield reconstruction is larger at far stations with a direction perpendicular to the wave propagation direction, then the reproducibility of the waveforms is significantly increased. In addition, the spatial gradients of the amplitudes are well reproduced by the optimized SWG method even though the optimization only focused on the amplitudes. Therefore, our proposed optimization scheme can be used to accurately estimate seismic wavefields in a nonuniformly distributed station array. Actually, the weighting functions optimized in this study succeeded to reconstruct the seismic wavefield of a shallow crustal earthquake that occurred around the Tokyo metropolitan area, based on the observed seismograms obtained by the MeSO-net.
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U2 - 10.1785/0220200196
DO - 10.1785/0220200196
M3 - Article
AN - SCOPUS:85105730502
SN - 0895-0695
VL - 92
SP - 2015
EP - 2037
JO - Seismological Research Letters
JF - Seismological Research Letters
IS - 3
ER -