Field observations indicate that a tidal salinity front that is regenerated each lower low water is a prominent feature of intertidal zone flow during wet winter months. A strong longitudinal density gradient at the front influences flow dynamics through tidal straining and baroclinic forcing. During each inundation period the salinity gradient disperses as it advects across the intertidal zone. The average longitudinal dispersivity estimated from observations is about 10 m2 s-1. A three-dimensional numerical model yields comparable estimates of tidally averaged dispersivity for an idealized bathymetry with a subtidal channel and intertidal shoals. The instantaneous dispersivity through the tidal cycle depends on both vertical and lateral shear in along-channel velocity. Dispersion due to vertical shear is greatest during stratified ebbs and inversely depends on tidal forcing; dispersion due to lateral shear results from bathymetric variability between channel and shoal and increases with tidal amplitude. Similarly, the along-channel residual velocity is a combination of baroclinic and frictional processes. Frictional effects dominate the depth-averaged residual such that net flow is upstream on the shoals and downstream in the channel; however, the frictional pattern is moderated by baroclinic forcing at the front. Although along-channel dynamics dominate, differential advection of the salinity front establishes lateral baroclinic circulation between channel and shoals. Lateral residual circulation is flood dominant with dense water moving out of channel near the bed and convergence from the shoals at the surface. At times near the front the lateral salt flux can significantly affect the salinity budget in the channel.