Quantification of Water and Salt Exchanges in a Tidal Estuary

A calibrated three-dimensional hydrodynamic model was applied to study subtidal water and salt exchanges at various cross sections of the Perdido Bay and Wolf Bay system using the Eulerian decomposition method from 6 September 2008 to 13 July 2009. Salinity, velocity, and water levels at each cross section were extracted from the model output to compute flow rates and salt fluxes. Eulerian analysis concluded that salt fluxes (exchanges) at the Perdido Pass and Dolphin Pass cross sections were dominated by tidal oscillatory transport F-T,F- whereas shear dispersive transport F-E (shear dispersion due to vertical and lateral shear transport) was dominant at the Perdido Pass complex, the Wolf-Perdido canal, and the lower Perdido Bay cross sections. The flow rate Q(F) and total salt transport rate F-S showed distinct variation in response to complex interactions between discharges from upstream rivers and tidal boundaries. Q(F) and F-S ranged from -619 m(3)s(-1) (seaward) to 179 m(3)s(-1) (landward) and -13,480-6289 kgs(-1) at Perdido Pass when river discharges ranged 11.0-762.5 m(3)s(-1) in the 2008-2009 simulation period.