To handle a slowness model containing large contrasts, my algorithm
uses a simplified finite difference version of Podvin and Lecomte (1991).
Therefore, the true slowness model is approximated by a discrete slowness model
that consists of constant slowness cells in polar coordinates.
I assume that the grid sizes are small so that each individual cell can
be treated as a small rectangle of by
.At the boundaries of each cell, the slowness function is generally
discontinuous. The interfaces of the slowness model are formed along
the boundaries of the cells. As we will see later in the examples,
this approximation is adequate for the traveltime calculation, but
inadequate for the amplitude calculation when slowness varies sharply.