Using the average directions of the main wave-fronts which approach the coa
st of Bahia State - coinciding with that of the main wind occurring in the
area - and of their periods, we define a wave climate model based on the co
nstruction of refraction diagrams. The resulting model of sediment transpor
t was able to reproduce, in a general way, the sediment dispersion patterns
furnished by geomorphic indicators of the littoral drift. These dispersion
patterns control the generation of different types of sediment accumulatio
ns and of coastal stretches under erosion. We demonstrate that the presence
of the Abrolhos and Corumbau Point coral reefs is an important factor cont
rolling the sediment dispersion patterns, since them act as a large protect
ion against the waves action.