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  • Contrary to the case of a strictly one-dimensional mixing model, where properties such as heat and buoyancy have the same vertical eddy diffusivity as the tracer so that their vertical fluxes are uniquely related, this model yields a relation betweenvertical buoyancy and heat fluxes and the tracer flux which depends on the relative magnitude of the isopycnal and cross-isopycnal diffusivities.
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