The hydrodynamic feasibility of a proposed third inlet to East Matagorda Ba
y, Texas, was examined by application of a two-dimensional, depth-averaged
hydrodynamic model. Wind-driven flows in this remote, shallow bay frequentl
y dominate the weak astronomical tide. The bay presently has two connection
s to the Gulf of Mexico, one through a short flood-relief channel and the o
ther through a long and circuitous navigation channel. The study had to con
sider whether installation of a third inlet would cause the relief channel
to close or increase the already strong current velocity in the navigation
channel that is a concern for boating safety. The model was calibrated with
measurements of wind, water level, and current taken in this study. It is
concluded that the new inlet will be ebb-dominated because of the wind-indu
ced current, and that the relief channel will not close in the presence of
the new inlet. In addition, the peak current at a critical maneuvering area
in the navigation channel that presently poses a hazard to vessel traffic
will be reduced by as much as 25% as a result of opening the new inlet.