Measurements obtained with a profiling laser-Doppler velocimeter revea
l the vertical structure of velocity in a wave boundary layer over a s
and beach during two periods of approximately stationary forcing, each
with a duration of several hours. The measurements indicate clearly t
he reduction in variance and the increase in phase, relative to the ov
erlying flow, that are expected in an oscillatory boundary layer. The
measurements also indicate a distortion of the mean alongshore velocit
y within the wave boundary layer, which has previously been predicted
theoretically and observed in laboratory experiments. The thickness an
d structure of the boundary layer are approximately consistent with co
mputations based on an existing eddy viscosity model, and model-based
best fit estimates of bottom roughness are approximately consistent wi
th existing semiempirical descriptions of wave-formed sand ripples.