Fig. 6From: Generation mechanism of large later phases of the 2011 Tohoku-oki tsunami causing damages in Hakodate, Hokkaido, JapanEigenfunctions, that is, the spatial distributions of the water heights, and eigen periods of the first mode (a), fundamental mode, and second mode (b) computed from actual bathymetry for Hakodate Bay. The red ellipse shows the Hakodate port area which is the most populated and famous tourist area in HakodateBack to article page