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Generation mechanism of large later phases of the 2011 Tohoku-oki tsunami causing damages in Hakodate, Hokkaido, Japan

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Figure

Fig. 1 The slip distribution of the 2011 Tohoku-oki earthquake (Fujii et al. 2011) used to compute tsunamis in this study
Fig. 2 Comparison of observed (blue) and computed (orange) tsunami waveforms by solving the linear shallow water equations at four tidegauges, in a Hakodate, b Tomakomai, c Tomakomai-nishi, and d Urakawa, shown in Fig
Fig. 3 Comparison of observed (blue) and computed (orange) tsunami waveforms by solving the non-linear shallow water equations with amoving boundary condition at the four tide gauges, in a Hakodate, b Tomakomai, c Tomakomai-nishi, and d Urakawa
Fig. 4 Snapshots of the tsunami height distribution around Hakodate taken 460, 480, 505, and 535 min after the earthquake, as shownin Fig
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