Fig. 5From: Performance of uniform and heterogeneous slip distributions for the modeling of the November 2016 off Fukushima earthquake and tsunami, JapanComparison of models A, B, C, and D at 13 stations. a Absolute amplitudes of the first pulling tsunami wave cycle. b Difference between the absolute amplitude of the computation and that of the observation. c Periods of the first wave cycle. d VR1. The dotted lines in b represent approximate best-fit curvesBack to article page