The Impact of Agulhas Leakage on the Atlantic Overturning Circulation

The Agulhas Current is the strong western boundary current of the South Indian Ocean. It flows southward along the east coast of southern Africa, but when it passes the southern tip of South Africa, it makes a tight turn (“retroflects”) and flows back into the Indian Ocean. However, this retroflection shortcuts every few months spawning a large column of warm and salty Indian Ocean water that drifts into the Atlantic. This process is called Agulhas Leakage (De Ruijter et al. 1999).

Studies using both conceptual 2D models (Weijer et al., 1999; Weijer et al., 2001) and a low-resolution GCM (Weijer et al., 2002) indicate that the interocean fluxes of heat and salt may exert a considerable influence on the strength and stability of the Atlantic overturning circulation. In the case of Agulhas Leakage, the salt and temperature anomalies initially cancel with respect to density. Rapid decay of the thermal anomaly leaves a density anomaly when the Indian Ocean water is advected northward. This results in a modification of the large-scale pressure distribution that tends to strengthen the overturning circulation. And since a stronger overturning circulation enhances advective feedbacks, it also becomes more stable with respect to large-amplitude perturbations.

This work was done in the group of Will de Ruijter, in collaboration with Henk Dijkstra and Peter Jan van Leeuwen, at IMAU.


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