Employing the Fresnel and Kirchhoff approximations in the Helmholtz integral equation and assuming a Gaussian correlation function, an equation can be derived that predicts the time distribution of the acoustic pressure from a pulse propagated over a rough bottom. A simple expression can be found that relates the half duration time of the pulse to the surface rms slope, grazing angle, and slant range. Applying this expression to a measured time series from a rough Pacific thin sediment area, the computed rms slope is found to be larger than that estimated by spectral means. This increase in slope value can be thought of as an ‘‘effective’’ slope, that is, this computed slope was obtained using a first-order scattering theory, and the increase must therefore be including second-order scattering effects. The size of the increase leads to the conclusion that in thin sediment areas, second-order scattering effects such as multiple scattering, layering resonances, and shadowing must be as important as first-order scattering. [Work supported by ONR-AEAS Program.]