Density Stratification, Turbulence, but How Much Mixing?

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Ocean Circulation Kinetic Energy: Reservoirs, Sources, and Sinks (2009, neutral): “Laboratory experiments are quite striking (e.g., Ivey et al., 2008, and references there), but field measurements at the much higher Reynolds numbers present in the open ocean would be welcome, as would laboratory studies of the boundary layers in the presence also of strong rotation.”
A diapycnal diffusivity model for stratified environmental flows (2013, methodology): “In previous parameterizations, the transition to the Molecular regime was assumed to occur at Reb = 7 for all Pr, based on data with Pr = 0.7 (SKIF; Ivey et al., 2008).”