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A Multi-Limit Mixed-Layer Entrainment Formulation
turbulence kinetic energy buoyancy flux density-fluctuation
2009/2/5
The second-moment equations for buoyancy flux and density-fluctuation variance in the entrainment zone of a mixed layer are combined to yield an entrainment rate (we dependence having the nature of Tu...
On the Ocean’s Large-Scale Circulation near the Limit of No Vertical Mixing
Large-Scale Circulation No Vertical Mixing Limit
2008/10/27
By convention, the ocean’s large-scale circulation is assumed to be a thermohaline overturning driven by the addition and extraction of buoyancy at the surface and vertical mixing in the interior. Pre...