Fig. 1From: Generation mechanism of large later phases of the 2011 Tohoku-oki tsunami causing damages in Hakodate, Hokkaido, JapanThe 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 middleBack to article page