Turbulence and mixing along a microtidal and stratified estuary-shelf transition

Abstract. This study investigates the hydrodynamic and mixing processes at the estuary–shelf transition of a microtidal system, and the buoyant plume generated at the Patos Lagoon mouth (Brazil). Using measurements of turbulent kinetic energy (TKE) dissipation (ϵ), current velocities, salinity, and temperature collected during a high-discharge period (∼9,400 m³ s^-1), we characterize the spatial evolution of turbulence and mixing along the channel, from the source to the buoyancy-driven plume region. Observations show that the jetty-constrained inlet acts as a morphological nozzle, forcing the flow to remain supercritical (Fri > 1) for several kilometres onto the inner shelf. Despite strong stratification, intense shear-driven turbulence was observed, with TKE dissipation rates (ε) reaching 10^-3 W kg^-1 near the mouth, comparable to values reported in high-energy mesotidal and macrotidal systems. Analysis of the buoyancy Reynolds number (Reb) and the gradient Richardson number (Ri) indicates that inertial forcing overcomes buoyancy suppression, maintaining a predominantly turbulent regime (Reb > 200) at the plume front. These results demonstrate that, in narrow, high-discharge estuarine outlets, morphological confinement and sustained supercritical flow govern the near-field evolution of buoyant plumes, maintaining vigorous mixing even under pronounced density stratification.