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Fig. 3 | Earth, Planets and Space

Fig. 3

From: Frequency-dependent amplification of the Sanriku tsunamis in Ryori Bay

Fig. 3

Comparison 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, respectively

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