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Ocean Science An interactive open-access journal of the European Geosciences Union
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Volume 6, issue 4
Ocean Sci., 6, 983–995, 2010
https://doi.org/10.5194/os-6-983-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Deep ocean exchange with the shelf

Ocean Sci., 6, 983–995, 2010
https://doi.org/10.5194/os-6-983-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.

  30 Nov 2010

30 Nov 2010

The influence of the Brazil and Malvinas Currents on the Southwestern Atlantic Shelf circulation

R. P. Matano1, E. D. Palma2,3, and A. R. Piola4,5 R. P. Matano et al.
  • 1College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon, USA
  • 2Departamento de Física, Universidad Nacional del Sur, Bahia Blanca, Argentina
  • 3Instituto Argentino de Oceanografía, CONICET, Bahía Blanca, Argentina
  • 4Departamento de Oceanografía, Servicio de Hidrografía Naval, Buenos Aires, Argentina
  • 5Departamento de Ciencias de la Atmósfera y los Océanos, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Argentina

Abstract. The oceanic circulation over the southwestern Atlantic shelf is influenced by large tidal amplitudes, substantial freshwater discharges, high wind speeds and – most importantly – by its proximity to two of the largest western boundary currents of the world ocean: the Brazil and Malvinas currents. This review article aims to discriminate the dynamical processes controlling the interaction between this extensive shelf region and the deep-ocean. The discussion is focused on two broad regions: the South Brazil Bight to the north, and Patagonia to the south. The exchanges between the Brazil Current and the South Brazil Bight are characterized by the intermittent development of eddies and meanders of the Brazil Current at the shelfbreak. However, it is argued that this is not the only – nor the most important – influence of the Brazil Current on the shelf. Numerical simulations show that the thermohaline structure of the South Brazil Bight can be entirely ascribed to steady state, bottom boundary layer interactions between the shelf and the Brazil Current. The Malvinas Current does not show the development of eddies and meanders, but its influence on the Patagonian shelf is not less important. Models and observations indicate that the Malvinas Current not only controls the shelfbreak dynamics and cross-shelf exchanges but also influences the circulation in the shelf's interior.

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