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Fig. 2 | Earth, Planets and Space

Fig. 2

From: Effects of water domains on seismic wavefields: A simulation case study at Taal volcano, Philippines

Fig. 2

Vertical velocity waveforms on water surfaces calculated with a structure composed of a flat water layer overlying a homogeneous half space. Solid and dotted lines indicate the waveforms calculated using FDM and DWM codes, respectively. Waveforms calculated with a water depth of 40 m (1 grid cell) at epicentral distances of 1 km (a) and 10 km (b) and a water depth of 160 m (4 grid cells) at epicentral distances of 1 km (c) and 10 km (d) are shown.

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