Fig. 2From: Generation mechanism of large later phases of the 2011 Tohoku-oki tsunami causing damages in Hakodate, Hokkaido, JapanComparison of observed (blue) and computed (orange) tsunami waveforms by solving the linear shallow water equations at four tide gauges, in a Hakodate, b Tomakomai, c Tomakomai-nishi, and d Urakawa, shown in Fig. 1Back to article page