Based on the formal derivation of the mild-slope equation (Smith & Spr
inks, 1975), the neglected 'forcing terms' are rederived. It is shown
that the slope terms are of order epsilon(2), which are negligible acc
ording to the mild-slope assumption, where epsilon = /del h//kh repres
ents the classical definition of small parameter for mild-slope. It is
found that the curvature terms depend not only on epsilon but also on
the wave frequency and the terms have considerable effect on wave pha
se in the lower range of wave frequencies. Therefore, in the broad wav
e spectrum case, the curvature terms discarded by Smith & Sprinks (197
5) are necessary to accurately predict waves over a bottom with severe
curvatures.