In this paper a coastal wave transformation model is presented. The im
plementation of different wave theories and the terms for refraction,
shoaling, bottom friction, percolation, viscous dissipation and wave b
reaking are described. A few trial runs of the model have been made wi
th various deep water wave characteristics. The change in characterist
ics of a shoreward propagating wave is as expected. A comparative stud
y of model derived wave heights with satellite altimeter wave heights
is also done. It is found that model derived wave heights follow the s
ame trend as altimeter wave heights; and thus confirms the validity of
the model for estimation of shallow water wave heights.