1DH Boussinesq Wave Module - Examples
101
Figure 4.70 Phase-averaged model results. Spatial variation of the undertow
Figure 4.71 Moving shoreline model results. Temporal variation of the vertical and
horizontal run-up height. The still water shoreline is located at x
r
= 23.3
m
The simulated shoreline motion is converted into a vertical and a horizontal
displacement as illustrated in Figure 4.71. The large displacement at time
approximately 12:00:20 is caused by the warm-up of the model and should
be disregarded. The shoreline motion is seen to oscillate around 0.02 m
To Next Page
Loading...