Implications of inertial subrange scaling for stably stratified mixing
G. D. Portwood, S. M. de Bruyn Kops, C. P. Caulfield

TL;DR
This paper investigates how inertial subrange scaling influences scalar mixing in stably stratified turbulence, proposing a model that links turbulence constants to mixing efficiency at high Reynolds numbers.
Contribution
It introduces a theoretical model connecting inertial subrange scaling to scalar mixing rates in stratified turbulence, validated by direct numerical simulations.
Findings
The relationship between active scalar and turbulence time scales depends on Kolmogorov and Oboukhov-Corrsin constants.
Turbulent mixing coefficient can be estimated using energy dissipation rates and a universal constant at high Reynolds numbers.
A new model for diapycnal mixing with robust theoretical parametrization is proposed.
Abstract
The effects of turbulent dynamic range on scalar mixing in stably stratified turbulence are investigated by an adaptation of the theoretical passive scalar modelling arguments of Beguier et al. (1978) and demonstrated statistically using direct numerical simulations of statistically stationary homogeneous stratified and sheared turbulence (SHSST). By analysis of inertial and inertial-convective subrange scaling, we show that the relationship between active scalar and turbulence time scales is predicted by the ratio of the Kolmogorov and Oboukhov-Corrsin constants provided there is sufficient scale separation for inertial and inertial-convective subrange scalings to be valid. With this analysis, we show that the turbulent mixing coefficient, , that is, within this context defined to be the ratio of available potential energy () and turbulent kinetic…
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