2017
DOI: 10.1063/1.5012546
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A new subgrid characteristic length for turbulence simulations on anisotropic grids

Abstract: Direct numerical simulations of the incompressible Navier-Stokes equations are not feasible yet for most practical turbulent flows. Therefore, dynamically less complex mathematical formulations are necessary for coarse-grained simulations. In this regard, eddy-viscosity models for Large-Eddy Simulation (LES) are probably the most popular example thereof. This type of models requires the calculation of a subgrid characteristic length which is usually associated with the local grid size. For isotropic grids this… Show more

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Cited by 38 publications
(31 citation statements)
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References 42 publications
(120 reference statements)
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“…8 has a similar form to the Clark model [cf. 1,37,38], but with a different coefficient (i.e., 1/2 instead of 1/12) due to the difference in filtering.…”
Section: Defining the Difference Between The Two Solutions Asmentioning
confidence: 99%
“…8 has a similar form to the Clark model [cf. 1,37,38], but with a different coefficient (i.e., 1/2 instead of 1/12) due to the difference in filtering.…”
Section: Defining the Difference Between The Two Solutions Asmentioning
confidence: 99%
“…One could also analyze the ability of the vortex-stretching-based nonlinear model to predict (coherent) flow structures, such as the Taylor-Görtler vortices that occur in spanwise-rotating planechannel flow (Dai et al 2016). Other points of interest for future studies could be adaptation of the vortex-stretching-based nonlinear model to simulate rotating turbulent flows from an inertial frame of reference, or adaptation of the subgrid characteristic length scale (see, e.g., Trias et al 2017). Finally, our results indicate that supplementing the scaled anisotropic minimum-dissipation model with the nonlinear term of the vortex-stretching-based nonlinear model is beneficial.…”
Section: Discussionmentioning
confidence: 99%
“…On the other hand, anisotropic filter lengths have been used in conjunction with anisotropic subgrid scale models (Bardina et al 1980(Bardina et al , 1983aAbbà et al 2017). See Trias et al (2017) and references therein, for a review of different length scales accounting for the anisotropy of the flow. Although successfully employed, these anisotropic filter sizes have been defined in a rather heuristic way.…”
Section: First-order Modellingmentioning
confidence: 99%