A western margin frontal zone is described, from measurements of temperature, salinity and currents, in a section taken with R/V "Prof. W. Besnard" in December 1980, crossing the shelf break border at latitude 26º30'S. The analyses of the sections showed consistently the occurrence of an ascension of the T and S isolines over the shelf break. Simultaneous current measurements showed a surface eddy structure with clockwise circulation and anti-clockwise circulation having a common stem over the break characterizing a shelf break upwelling.
Water temperature; Salinity; Current measurement; Coastal upwelling; Oceanic eddies; Frontal zones; Oceanic fronts; Advection; Southeast coast-Brazil; R/V "Prof. W. Besnard"; Paranaguá; Continental shelf break