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Fig. 1 | Progress in Earth and Planetary Science

Fig. 1

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

Fig. 1

The slip distribution of the 2011 Tohoku-oki earthquake (Fujii et al. 2011) used to compute tsunamis in this study. The diamonds show the locations of the four tide gauges, that is, Hakodate, Tomakomai, Tomakomai-nishi, and Urakawa, to compare the observed and computed tsunami waveforms. The original tsunami waveform (without tide removal) observed in Hakodate (Japan Meteorological Agency 2012) is displayed in the middle

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