Waterhouse, A. F., University of Florida, Gainesville, USA, email@example.com
Valle-Levinson, A. ., University of Florida, Gainesville, USA, firstname.lastname@example.org
SPATIAL STRUCTURE OF TIDAL AND RESIDUAL FLOWS AT A TIDAL INLET
Located on the northeastern coast of Florida, Ponce Inlet is a shallow, short estuary with depths ranging between 2m in the shallows up to 10m in the thalweg. Current speeds, surface and profiling measurements of conductivity, temperature and depth were collected over a semi-diurnal tidal cycle on September 5, 2007. The mean flow in this estuary agrees with the flow structure of tidally dominated residual flow: inflow in the deeper channel and outflow through the shallower shoals. However, lateral gradients in density with values close to 0.01 kg/m^4 are observed during ebb but become negligible during flood. The importance of the forcing caused by the ebb-tide density gradient relative to tidal influence and bathymetric effects are assessed.
Presentation is given by student: Yes
Time: 17:30 - 19:30