Measured free surface elevations and horizontal velocities of non-breaking
regular waves on a 1:2 rough permeable slope are analyzed to examine the cr
oss-shore variations of the incident and reflected waves on the steep slope
. The co-located measurements of the free surface elevation and horizontal
Velocities at a number of elevations are used to separate the incident and
reflected waves locally. The estimated partial standing waves are then show
n to describe the local free surface elevation and horizontal velocity reas
onably well. The incident wave energy flux is found to be approximately con
stant along the 1:2 slope, whereas the data and linear theory are not accur
ate enough to detect the cross-shore Variation of the relative small wave r
eflection coefficient. The measured mean horizontal velocities are shown to
be in qualitative agreement with the return current estimated from the sep
arated incident and reflected waves.