4.5 Article

An Optimum 2D Seismic-Wavefield Reconstruction in Densely and Nonuniformly Distributed Stations: The Metropolitan Seismic Observation Network in Japan

Journal

SEISMOLOGICAL RESEARCH LETTERS
Volume 92, Issue 3, Pages 2015-2027

Publisher

SEISMOLOGICAL SOC AMER
DOI: 10.1785/0220200196

Keywords

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Funding

  1. Japan Science and Technology Agency (JST) Core Research for Evolutional Science and Technology (CREST) program [JPMJCR1763]
  2. Japan Society for the Promotion of Science (JSPS) [JP19K04006]

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An optimization method for applying the seismic-wave gradiometry method to a dense seismic station network with nonuniformly distributed seismographs was proposed, focusing on the Metropolitan Seismic Observation Network (MeSO-net) in Tokyo. Through numerical investigation, optimal shapes of weighting functions were found to greatly improve the reproducibility of seismic wavefields, especially when considering the direction of wave propagation.
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 the weight 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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