A simple model of open coastal dynamics is adapted to provide an analy
tic solution of the vertical and axial structure of tidal currents in
an estuary. Applied to the Hey River estuary in northern Queensland, t
he model provides an accurate representation of the four major tidal c
onstituents. By best-fit analysis of the model results to data from th
ree current meters, the vertical eddy viscosity for the estuary is est
imated as 2.8 x 10(-3) m2 s-1, and the linear friction coefficient as
8 x 10(-4) ms-1. Bottom boundary considerations indicate that the data
are consistent with the concept of a bottom logarithmic layer 0.6 m d
eep, in which the eddy viscosity increases linearly from near-zero to
its free-stream value.