Fig. 3From: Effects of water domains on seismic wavefields: A simulation case study at Taal volcano, PhilippinesSnapshots of synthetic velocities V y (upper panels) and V z (lower panels) at half grids below the land and water surfaces at t = 3, 5, 7, and 9 s calculated with the water model using T p = 2 s and a source at 220 m below sea level.Back to article page