Two-dimensional changes of beach profile are computed by the continuit
y equation of sediment. Wave transformation used in the continuity equ
ation is obtained by solving the shallow water equations numerically.
The application of this method for different wave height, period, and
sand particle diameters shows that this approach is reasonable. Applyi
ng this method and the result of field observations to Nakisuna beach,
the coastal changes there are found to be stable without any protecti
on.