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Additional file 1: Figure S1. Bathymetric (10-m contour interval) and topographic maps of the waveform comparison sites (red stars; see red squares in Fig. 1) for the tsunami calculations. Figure S2. Calculated tsunamis generated by landslide sources in the northern part of the bay. The results (models A, left; and B, right) are shown. a Comparison between calculated (red curves) and observed waveforms (black curves, video-inferred waveforms from Carvajal et al. 2019; gray curve, waveform at the Pantoloan tide gauge). b Distributions of the maximum calculated tsunami amplitude over the entire bay for each fault model. The color scale indicates the tsunami amplitude. Left and right graphs compare the calculated tsunami run-up heights (red curves) with those (black bars) determined by field surveys on the western and eastern coasts, respectively. Figure S3. Calculated tsunamis generated by landslide sources in the southern part of the bay. The results (models D, left; and F, right) are shown. Same as Figure S2 for source models D and F. Figure S4. Comparison of calculated and observed run-up heights. The heights on the eastern (blue) and western coasts (green) for model G are shown. Aida’s (1978) K and κ were calculated from these data and are reported for each coast as well as for all sites (black). The solid and dashed lines indicate the ratio of 1.0 between the calculated and observed run-up heights and the ratios of 2.0 and 0.5, respectively. Figure S5. Calculated tsunamis generated by a coastal collapse and Takagi et al. (2019) (models N and O). Same as Figure S2 for source models N and O. |
