Figure 1 | Scientific Reports

Figure 1

From: Frequency dispersion amplifies tsunamis caused by outer-rise normal faults

Figure 1

Non-dispersive (blue) and dispersive (red) propagation of Gaussian soliton wave shapes. (a) A positive (upwardly convex) incident wave. (b) A negative (downwardly convex) incident wave. The waves propagate in the horizontal direction over a water depth of 4000 m. Dispersion creates wave trains and increases the wave height in (b). Movie S1 shows propagations of the waves.

Back to article page