Velocity data from 28 degrees N, 84 degrees W on the west Florida cont
inental shelf are presented. The data were sampled from October 1993 t
hrough January 1995 at 1 m intervals between 3 m and 42 m in a total w
ater depth of 47 m. Their monthly means suggest an annual cycle hypoth
esized to be driven by a seasonally varying shelf-wide baroclinic stru
cture. Motions at semi-diurnal, diurnal and synoptic time scales are s
easonally modulated, both by wind forcing and stratification that deco
uples fluid motions from the damping effects of bottom friction. These
motions are presented in the form of progressive vector plots. With 1
6 months of data, probability density and distribution functions for a
long-shore and across-shore particle displacements over specific time
intervals are constructed. For daily intervals, particles are equally
likely to travel approximately 5 km (depending upon confidence interva
l) in any direction. For monthly intervals, particles may travel a few
hundred km, primarily along-shore.