Meanders and Rings

The combined float/SSH data set enabled us to continuously observe the evolution of mesoscale features in the greater Agulhas region, results of which are discussed for the major mesoscale events known for the region-- Agulhas Rings, Agulhas Current Meanders, and Natal Pulses.

Agulhas Rings

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During the 3 year experimental period we observed 16 rings to drift through the Cape Basin. This number is at the lower end of earlier estimates (4-9 per year, [Lutjeharms, 1996]), however the identification of a ring shedding event is inherently difficult, due to numerous rings reattaching to the Agulhas Retroflection or merging together during their early stage. The phase propagation of the positive SSH anomalies associated with rings was 5.2 ± 1.7 cm s-1, which is lower than estimates in the literature (6-9 cm s-1, [Olson and Evans, 1986]).

Agulhas Current Meanders

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5 major Agulhas Current meanders translated south-westward along the continental shelf break at similar speeds, averaging to 11.6 ± 0.8 cm s-1. This is in contrast to earlier observations by other authors [Lutjeharms and Roberts, 1988], who found a propagation speed of 15-20 cm s-1 for the region northeast of Port Elizabeth and 5-6 cm s-1 to the southwest of Port Elizabeth.

Eddies embedded in major meanders of the Agulhas were shed from their captured position between the coast and the Agulhas Current at the southernmost tip of the Agulhas Bank. In all cases this involved a pinching off of a juvenile Agulhas Ring, which is why the region adjacent to the tip of the Agulhas Bank can be viewed as a crossroad in which Agulhas rings translate north-westward and cyclonic eddies drift west- or south-westward.

Natal Pulses

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The total number of shelf-trapped cyclonic events (11 in 3 years) is similar to earlier estimates of Natal Pulse frequency (14 in 4 years [de Ruijter et al., 1999]). Most of the meanders we resolved were only discernable from Port Elizabeth downstream. This is in contrast to the concept that all major meanders, Natal Pulses, are formed in the Natal Bight.

PROBLEM RAFOS FLOATS MEAN FIELD MESOSCALE MEANDERS AND RINGS
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