Abstract

Between 1975 and 1978, eight cruises were executed off the South African east coast to determine the volume transport of the Agulhas Current. The results at 31°S indicate that the average geostrophic transport relative to 1000 m was 30 × 10 6 m 3 s −1; by matching the geostrophic current profiles to observed currents near the surface, a volume transport of 62 × 10 6 m 3 s −1 is obtained in the upper 1000 m. Indications are that the volume transport of the current increases downstream by 6 × 10 6 m 3 s −1 per 100 km.

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