Editorial Type:
Article
Article Type:
Research Article

Circulation and Variability at the Southern Boundary of the Brazil Basin

Nelson G. Hogg Woods Hole Oceanographic Institution, Woods Hole, Massachusetts

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Gerold Siedler Institut für Meereskunde an der Universität Kiel, Kiel, Germany

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Walter Zenk Institut für Meereskunde an der Universität Kiel, Kiel, Germany

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Print Publication:
01 Feb 1999
DOI:
https://doi.org/10.1175/1520-0485(1999)029<0145:CAVATS>2.0.CO;2
Page(s):
145–157
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Abstract

As a contribution to the WOCE Deep Basin Experiment, an array of current meters with individual record lengths exceeding 1½ years was set across the southern boundary of the Brazil Basin between early 1991 and early 1996. The array spanned the Santos Plateau, the Vema Channel, and the Hunter Channel, all areas believed to be important for transport of Antarctic Bottom Water between the Argentine and Brazil Basins. From the combination of geostrophic velocities computed from hydrographic stations and those directly measured, the total transport of bottom water (potential temperature below 2°C) is estimated to be about 6.9 Sv (Sv ≡ 106 m3 s−1) northward, with about 4 Sv coming through the Vema Channel and the remainder through the Hunter Channel.

Properties of the eddy field are also discussed. Eddy energy levels and their spatial distribution are similar to comparable regimes in the North Atlantic. Integral timescales vary from a few days to several weeks with distance from the Brazil Current and the western boundary. The eddy heat flux is in the same direction as the heat advection by the mean flow but considerably smaller.

Corresponding author address: Nelson G. Hogg, Clark Laboratory 3, Mail Stop #21, Woods Hole Oceanographic Institution, Woods Hole, MA 02543-1541.

Abstract

As a contribution to the WOCE Deep Basin Experiment, an array of current meters with individual record lengths exceeding 1½ years was set across the southern boundary of the Brazil Basin between early 1991 and early 1996. The array spanned the Santos Plateau, the Vema Channel, and the Hunter Channel, all areas believed to be important for transport of Antarctic Bottom Water between the Argentine and Brazil Basins. From the combination of geostrophic velocities computed from hydrographic stations and those directly measured, the total transport of bottom water (potential temperature below 2°C) is estimated to be about 6.9 Sv (Sv ≡ 106 m3 s−1) northward, with about 4 Sv coming through the Vema Channel and the remainder through the Hunter Channel.

Properties of the eddy field are also discussed. Eddy energy levels and their spatial distribution are similar to comparable regimes in the North Atlantic. Integral timescales vary from a few days to several weeks with distance from the Brazil Current and the western boundary. The eddy heat flux is in the same direction as the heat advection by the mean flow but considerably smaller.

Corresponding author address: Nelson G. Hogg, Clark Laboratory 3, Mail Stop #21, Woods Hole Oceanographic Institution, Woods Hole, MA 02543-1541.

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