The linear theory for waves impinging obliquely on a vertical, porous
breakwater with an impermeable crown is examined. The wave-induced flo
w within the breakwater is modeled by the 1972 theory of Sollitt and C
ross. Using eigen-function expansions for the velocity potentials seaw
ard of the breakwater, beneath the crown, and behind the structure, th
e reflection and transmission coefficients are calculated to determine
the sheltering provided by the breakwater. The results agree well wit
h other methods, including a plane wave analysis. obtained by neglecti
ng the evanescent wave modes. The distribution of the wave-induced pre
ssure along the base of the crown is also calculated, showing that the
linear pressure gradient assumption usually applied for uplift forces
on the breakwater crown is inaccurate.