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Gokhan Danabasoglu, Susan C. Bates, Bruce P. Briegleb, Steven R. Jayne, Markus Jochum, William G. Large, Synte Peacock, and Steve G. Yeager

-adiabatic ocean interior and is not valid near the boundaries. A practice has been to taper the effects of parameterized eddy fluxes as the boundaries are approached. This approach is not physical, particularly near the surface where diabatic mesoscale fluxes may dominate mixing. We include the effects of these diabatic mesoscale fluxes within the surface diabatic layer, using a simplified version of the near-boundary eddy flux parameterization of Ferrari et al. (2008) , as implemented by Danabasoglu et al

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