Tsunami generated in scenarios A are considered to be the
worst case. However, it is more probable for the subduction zone
to break at lower slip magnitudes, for instance 25%, 50% and 75%
of the original values indicated in Fig. 2. Respective simulated wave
height at observation points around SCS are shown in Fig. 6 and
Table 3. There is just a little change in arrival time between the extreme
earthquake and small ones, which is expected from the
established fact that the nonlinear phenomenon is not very prominent
for offshore tsunami (Dao and Tkalich, 2007). This leads also
to almost linear change of wave height according to the scale of the
slip magnitude, which is observed in Fig. 7.