In April 1982, an oceanographie investigation was conducted off the Brazilian coast in order to obtain the spatial characteristics of the thermal structure and to locate the Brazil Current flow both north and south of the seamount chain at 20º30'S. Dining the survey, remote sensing satellite data were also obtained on several occasions to assist in the delineation of the surface thermal structure. A 23ºC thermostad was observed along most sections. Along sections with stronger baroclinic signatures, such as the one in Cabo Frio, the thermostad seems to be pinched off somewhat similar to the pinching off the 18ºC water in the Gulf Stream North wall. The current structure and volume transports, relative to the 500 dbar isobaric surface, were calculated using both hydrographie station data and the closely spaced XBT measurements. A comparison of these results, for the data observed along the section of Cabo Frio, indicates that some details of the geostrophic currents are lost when the hydrographie data are used; the corresponding volume transports agree within 17% (33 Sv using hydrographie data against 2.8 Sv using XBT data). A volume transport budget, obtained through the transport computation along all sections between 19º and 22ºS, indicates that the Brazil Current appears to flow through the passage between the most inshore banks and not to the east. The net volume transport (2.9 Sv) is in close agreement with the Cabo Frio section volume transport, where the total flow of the Brazil Current was supposedly bracketed by the station sampling.
Water circulation; Brazil Current; Thermal structure; T/S diagrams; Geostrophic currents; Cabo Frio; Bancos de Abrolhos