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

<p>The simulation results used in the submitted manuscript</p> <p>Simulation results of high-frequency T-wave propagation from regions near the Sofug seamount and the Sumisu Caldera</p> <ul> <li>sac.tar: envelopes of simulation results</li> <li>green_sofugan: source grids and index information for simulation results in the region near the Sofugan Volcano</li> <li>green_sumisu: source grids and index information for simulation results in the region around the Sumisu Caldera</li> </ul> <p>The characteristics of simulated envelopes were listed in 231009GF_M.KMB06_???.dat (near the Sofu seamount) and 180506GF_M.KMB06_???.dat (Sumisu Caldera).</p> <ul> <li>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</li> </ul> <p>Details are described in "<span>Takemura,&nbsp;S.</span>,&nbsp;<span>Kubota,&nbsp;T.</span>, &amp;&nbsp;<span>Sandanbata,&nbsp;O.</span>&nbsp;(<span>2024</span>).&nbsp;<span>Successive tsunamigenic events near Sofu Seamount inferred from high-frequency teleseismic&nbsp;<em>P</em>&nbsp;and regional&nbsp;<em>T</em>&nbsp;waves</span>.&nbsp;<em>Journal of Geophysical Research: Solid Earth</em>,&nbsp;<span>129</span>, e2024JB029746.&nbsp;<a href="https://doi.org/10.1029/2024JB029746">https://doi.org/10.1029/2024JB029746</a>"</p>