Fig. 8From: Short-wave run-ups of the 1611 Keicho tsunami along the Sanriku CoastSimulated inundation area (blue) under the scenario with sources N and S, and a comparison of the simulated heights and observations. The simulated heights are displayed to follow the observed values from the observation sites (red circle) in (a). The magnitude of the error in (b) is the one shown in Ebina and Imai (2014), and the gray area indicates an error range within 50%Back to article page