We conduct a parametric study of diapycnal mixing using one-dimensional-turbulence (ODT) simulations. Homogeneous sheared stratified turbulence is considered. ODT simulations reproduce the intermediate and energetic regimes of mixing, in agreement with previous work, but do not capture important physics of the diffusive regime. ODT indicates for the intermediate regime, and for the energetic regime and limit of near-zero stratification. Here is the turbulent diffusivity for mass, the dissipation rate, N the buoyancy frequency, and h the computational domain height, where h is relevant mainly in simulations with jump-periodic vertical boundary conditions. These scaling relationships suggest that is independent of the molecular diffusivity. ODT results for a wide range of parameters show that cannot be parametrized solely with the turbulent intensity parameter , in contrast with the previous studies, but it is well predicted by correlations using the Ellison length scale.
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Research Article|
May 27 2011
Vertical mixing in homogeneous sheared stratified turbulence: A one-dimensional-turbulence study
Esteban D. Gonzalez-Juez;
Esteban D. Gonzalez-Juez
a)
1Combustion Research Facility, Sandia National Laboratories, Livermore, California 94551,
USA
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Alan R. Kerstein;
Alan R. Kerstein
b)
1Combustion Research Facility, Sandia National Laboratories, Livermore, California 94551,
USA
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Lucinda H. Shih
Lucinda H. Shih
2Contra Costa Water District, Concord, California 94520,
USA
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a)
Electronic mail: [email protected].
b)
Electronic mail: [email protected].
Physics of Fluids 23, 055106 (2011)
Article history
Received:
November 08 2010
Accepted:
April 21 2011
Citation
Esteban D. Gonzalez-Juez, Alan R. Kerstein, Lucinda H. Shih; Vertical mixing in homogeneous sheared stratified turbulence: A one-dimensional-turbulence study. Physics of Fluids 1 May 2011; 23 (5): 055106. https://doi.org/10.1063/1.3592329
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