Acoustic Doppler current profiles were measured for a twelve-hour period on
February 21, 1997 across Thimble Shoal channel, lower Chesapeake Bay, for
the purpose of determining bathymetrically-induced spatial gradients in the
flow and their implications for the lateral momentum balance in estuaries.
A least-squares fit to semidiurnal and quarter-diurnal harmonics was used
to separate the tidal and subtidal contributions to the observed flow. The
period of observation was characterized by onshore winds and subtidal inflo
w everywhere along the transect sampled but strongest in the channel. Spati
al gradients in both the tidal and subtidal horizontal flows showed that th
e greatest lateral shears and convergences were found where the bathymetric
changes were sharpest, i.e., on the shoulders of the channel. The ratio of
the quarter-diurnal to the semidiurnal tidal amplitudes was greatest over
the channel shoulders, for both the along- and across-estuary flow componen
ts, and indicated the importance of non-linear effects there. The nonlinear
term caused by across-estuary divergence was larger than the Coriolis term
over the channel shoulders. The nonlinear contribution was comparable to t
he Coriolis acceleration in the subtidal and tidal lateral momentum balance
s. For the tidal balance, the local accelerations were also as important as
the Coriolis accelerations. Equivalent results in the momentum balances we
re obtained with another data set of October 1993. Contrary to the customar
y assumption, the across-estuary momentum balance in this area was ageostro
phic.