Research news on estuarine mixing

Estuarine mixing refers to the set of physical and biogeochemical processes that govern the blending of riverine freshwater with saline coastal ocean water in estuaries, creating strong horizontal and vertical gradients in salinity, temperature, and suspended material. It is controlled by tidal forcing, river discharge, stratification, turbulence, Coriolis effects, and basin geometry, and is commonly categorized into well-mixed, partially mixed, and highly stratified (salt wedge) regimes. Estuarine mixing regulates density structure, circulation patterns, residence times, and material fluxes, thereby strongly influencing nutrient distributions, contaminant transport, primary productivity, and the transformation and retention of terrestrial and marine inputs.