Journal of Geophysical Research Atmospheres · 1987 · 47 citations · 20 references
Natural SciencesEarth SciencesPhysicsDynamic MeteorologyFluid DynamicsOcean MixingStratified FlowTurbulenceTurbulent FlowTurbulent FluxesTurbulent MixingVertical MixingDissipation RateGradient Richardson NumberMixing EfficiencyMomentum FluxesRichardson NumberStratified TurbulenceTurbulent Dissipation RatesTurbulent Mixing Length Scales
Nearly steady state mixing efficiencies, as characterized by the flux Richardson number R f , have been measured in stably stratified, turbulent, uniform gradient shear flows. The turbulent dissipation rate ϵ, the vertical mass and momentum fluxes and , and the mean and rms density and velocity fluctuations were obtained from simultaneous single point measurements of velocity and density. R f and the gradient Richardson number Ri were calculated at a number of positions in the spatially evolving shear flow. Within the investigated range of stabilities 0.02< Ri <0.08, R f was observed to increase with Ri . It is found that the length scale arguments successfully applied by Rohr et al . (1984) to the case of decaying, stably stratified, unsheared grid turbulence can also account for the overall behavior of the mixing efficiency ( R f ) as a function of stability ( Ri ) in the present case of growing, stably stratified, uniform mean shear turbulence.
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Evolution of Physical Oceanography
P J Dobson · Physics Bulletin · 1982 · 675 citations
Experiments on nearly homogeneous turbulent shear flow
F. H. Champagne, V. G. Harris, S. Corrsin · Journal of Fluid Mechanics · 1970 · 475 citations