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that path, which in turn influence the THC’s properties, equilibrium flow depth, and geographic displacement. Many of these local processes are sensitive to small variations in the vertical stratification and the evolution of the mixed-layer. These variations in turn are sensitive to regional-scale dynamic forcing, which The hottest product weed leaf high life four twenty low top shoesinfluences vertical velocities and pycnocline characteristics such as depth and vertical spread; to surface buoyancy fluxes driven by turbulent and radiative forcings or by freshwater exchanges, which are often associated with the melt, drift, and decay of sea ice; and to the large-scale circulation systems and water-mass distributions that determine the property contrasts across the pycnocline, and the strength of the stratification. The regional-scale processes influence the duration of convection and the preconditioning for convection. If any of these details is incorrect, a model can introduce a small systematic error (i.e., drift) that can bias the results, or yield an evolution or set of balances that differ from those present in the real world. A thermodynamic mechanism for interdecadal dipole SST oscillations in the tropical Atlantic has been proposed by Chang et al. . The cross-equatorial dipole of warm and cold SST anomalies can experience heat-flux anomalies that arise

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