High-frequency shallow-water reverberation statistics were measured fr
om a smooth, sandy, featureless seafloor. The reverberation statistics
are presented as a function of source frequency (20-180 kHz), grazing
angle (30-degrees, 20-degrees, 9.5-degrees) and source beamwidths (1.
2-degrees-2.75-degrees). Generally, the reverberation statistics did n
ot follow a Rayleigh fading model. The model dependence of the reverbe
ration statistics exhibited a complex behavior that ranged from near G
aussian to beyond log-normal. The results show that small changes in t
he source frequency, grazing angles, and beamwidths caused large varia
tions in the model dependence of the reverberation statistics.