Fig. 7From: Frequency-dependent amplification of the Sanriku tsunamis in Ryori BayThe temporal tsunami waveforms during the primary wave along the control line specified in Fig. 1b. The horizontal distance is positive towards the offshore from site B. The dotted, dashed, and solid lines represent the waveforms observed at times τ = τ0, τ0 + dτ, and τ0 + 2dτ; dτ is 150 s and τ0 for the 2011, 1933, and 1896 tsunamis are 1560, 2010, 1605 s, respectivelyBack to article page