Fig. 5From: Evaluation of accuracy of synthetic waveforms for subduction-zone earthquakes by using a land–ocean unified 3D structure modelNormalized, real part of rigidity kernels for period of a 12.8 s, and b 6.1 s, for the vertical component at station TYS (F-net). Crosses on the top map denote the locations of the FAMT solution (SRC) and the station (TYS), respectively. The horizontal slices of the three-dimensional kernels at depths of 2, 11, 21, and 30 km are displayed. The kernels are smoothed using a running average with a cell of \(11.7 \times 11.7\) km horizontally and 6.3 km vertically, normalized with the maximum amplitude for each period, and clipped at a normalized amplitude of \(\pm \;0.5\)Back to article page