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from and are sustained by wind-induced latent-heating anomalies. This positive feedback is countered by a negative feedback that is provided by the advection of heat by the south-to-north flow of the North Brazil Current, the principal cross-equatorial warm current of the THC. This current provides oppositely signed SST (heat-content) anomalies that reverse the atmospheric-circulation anomalies, and then remove the SST anomalies by reversing the evaporative heat-flux anomalies. An alternate mechanism to this cross-equatorial negative feedback has been proposed by Zhou . He suggests that the negative feedback is provided by the action of The hottest product weed leaf high life four twenty full printing low top shoesaltered winds, which produce SST anomalies that have opposite signs in lower and higher tropical latitudes. When these anomalies are advected by the surface circulation; they eventually restructure the atmosphere to yield anomalies with the opposite sign, again producing an interdecadal oscillation. Tourre et al. propose a third mechanism, involving flexure of the thermocline. uptake via the solubility pump. The stabilization also reduces

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