Two phenomenological constants explain similarity laws in stably stratified turbulence.
Two phenomenological constants explain similarity laws in stably stratified turbulence.
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DOI:
10.1103/physreve.89.023007
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发表时间:
2013-12
期刊:
影响因子:
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通讯作者:
G. Katul;A. Porporato;Stimit Shah;E. Bou‐Zeid
中科院分区:
文献类型:
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作者:
G. Katul;A. Porporato;Stimit Shah;E. Bou‐Zeid
In stably stratified turbulent flows, the mixing efficiency associated with eddy diffusivity for heat, or equivalently the turbulent Prandtl number (Pr(t)), is fraught with complex dynamics originating from the scalewise interplay between shear generation of turbulence and its dissipation by density gradients. A large corpus of data and numerical simulations agree on a near-universal relation between Pr(t) and the Richardson number (R(i)), which encodes the relative importance of buoyancy dissipation to mechanical production of turbulent kinetic energy. The Pr(t)-R(i) relation is shown to be derivable solely from the cospectral budgets for momentum and heat fluxes if a Rotta-like return to isotropy closure for the pressure-strain effects and Kolmogorov's theory for turbulent cascade are invoked. The ratio of the Kolmogorov to the Kolmogorov-Obukhov-Corrsin phenomenological constants, and a constant associated with isotropization of the production whose value (= 3/5) has been predicted from Rapid Distortion Theory, explain all the macroscopic nonlinearities.