Published June 17, 2024 | Version v1
Dataset Open

Simualtion results of T wave proapgation from regions near the Sofu seamount and the Sumisu Caldera

Authors/Creators

  • 1. Earthquake Research Institute, the University of Tokyo

Contributors

  • 1. National Research Institute for Earth Science and Disaster Resilience (NIED)
  • 2. Earthquake Research Institute, the University of Tokyo

Description

The simulation results used in the submitted manuscript

Simulation results of high-frequency T-wave propagation from regions near the Sofug seamount and the Sumisu Caldera

  • sac.tar: envelopes of simulation results
  • green_sofugan: source grids and index information for simulation results in the region near the Sofugan Volcano
  • green_sumisu: source grids and index information for simulation results in the region around the Sumisu Caldera

The characteristics of simulated envelopes were listed in 231009GF_M.KMB06_???.dat (near the Sofu seamount) and 180506GF_M.KMB06_???.dat (Sumisu Caldera).

  • longitude, latitude, depth, epicental distance, theoretical P traveltime, peak arrival time of body wave, theoretical T traveltime, peak arrival time of T wave, half-value starting, half-value ending, mximuma body wave amplitude, maximum T wave amplitude, envelope file name

Details are described in "Takemura, S., Kubota, T., & Sandanbata, O. (2024). Successive tsunamigenic events near Sofu Seamount inferred from high-frequency teleseismic P and regional T waves. Journal of Geophysical Research: Solid Earth, 129, e2024JB029746. https://doi.org/10.1029/2024JB029746"

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