Fig. 6From: Frequency-dependent amplification of the Sanriku tsunamis in Ryori Baya The incident waveforms based on Eq. (1) with α = 1 and 2; b the simulated run-up heights based on the incident waveforms with A0 = 3 m; c the simulated run-up heights based on the incident waveforms with A0 = 4 mBack to article page