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Patos Lagoon outflow within the Río de la Plata plume using an airborne salinity mapper: Observing an embedded plume
Authors:Derek Burrage  Joel Wesson  Carlos Martinez  Tabare Pérez  Osmar Möller Jr  Alberto Piola
Institution:1. Ocean Sciences Branch, Naval Research Laboratory (NRL), Stennis Space Center, MS 39529, USA;2. Programa de Ciencias del Mar y de la Atmosfera (PCMYA), Seccion Oceanologia, Facultad de Ciencias, Universidad de la Republica, Uruguay;3. Division de Investigacion y Desarrollo, CITMPSA, Montevideo, Uruguay;4. Fundação Universidade Federal do Rio Grande(FURG), Campus Carreiros, 96201-900 Rio Grande, RS, Brazil;5. Departamento Oceanografia, Servicio de Hidrografia Naval, Ciudad Autonoma de Buenos Aires, Buenos Aires, Argentina
Abstract:Major river systems discharging into continental shelf waters frequently form buoyant coastal currents that propagate along the continental shelf in the direction of coastal trapped wave propagation (with the coast on the right/left, in the northern/southern hemisphere). The combined flow of the Uruguay and Paraná Rivers, which discharges freshwater into the Río de la Plata estuary (Lat. ∼36°S), often gives rise to a buoyant coastal current (the ‘Plata plume’) that extends northward along the continental shelf off Uruguay and Southern Brazil. Depending upon the prevailing rainfall, wind and tidal conditions, the Patos/Mirim Lagoon complex (Lat. ∼32°S) may also produce a freshwater outflow plume that expands across the inner continental shelf. Under these circumstances the Patos outflow plume can be embedded in temperature, salinity and current fields that are strongly influenced by the larger Plata plume. The purpose of this paper is to present observations of such an embedded plume structure and to determine the dynamical characteristics of the ambient and embedded plumes.
Keywords:Sea water  Salinity  Surface temperature  Ocean circulation  River plumes  Oceanic fronts  Microwave remote sensing
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