Fig. 3From: Frequency-dependent amplification of the Sanriku tsunamis in Ryori BayComparison of the simulated run-up heights and the observed ones. a The results based on the computation domain with 6-m resolution and b the results based on the computation domain with 12-m resolution. Black, blue, and red correspond to the 2011, 1933, and 1896 tsunamis, respectively; filled circles and open circles indicate, respectively, the simulation results using the incident waveforms estimated by the linear long-wave model and the linear Boussinesq model. The solid line and the dashed lines indicate 0% and 25% errors, respectivelyBack to article page