## Abstract Large eddy simulation (LES) is based on separation of variable of interest into two parts—resolved and subgrid. The resolved part is obtained numerically using modified transport equation while the effect of the subgrid part is modelled using subgrid‐scale (SGS) models. In this paper we
Influences of subgrid scale dynamics on resolvable scale statistics in large-eddy simulations
✍ Scribed by Thierry Dubois; François Jauberteau; Ye Zhou
- Publisher
- Elsevier Science
- Year
- 1997
- Tongue
- English
- Weight
- 928 KB
- Volume
- 100
- Category
- Article
- ISSN
- 0167-2789
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✦ Synopsis
Recently, the e-expansion and recursive renormalization group (RNG) theories as well as approximate inertial manitblds (AIM) have been exploited as means of systematically modeling subgrid scales in large-eddy simulations (LES). Although these theoretical approaches are rather complicated mathematically, their key approximations can be investigated using direct numerical simulations (DNS). In fact, the differences among these theories can be traced to whether they retain or neglect interactions between the sabgrid-subgrid and subgrid-resolvable scales. In this paper, we focus on the influence of these two interactions on the evolution of the resolvable scales in LES: the effect A which keeps only the interactions between the small and large scales; and, the effect B which, on the other hand, keeps only the interactions among the subgrid-subgrid scales. The performance of these models is analyzed using the velocity fields of the direct numerical simulations. Specifically, our comparison is based on the analysis of the energy and enstrophy spectra, as well as higher-order statistics of the velocity and velocity derivatives. We found that the energy spectrum and higher-order statistics for the simulations with the effect A (referred to, hereafter, as model A) are in very good agreement with the filtered DNS. The comparison between the computations with effect a (referred to, hereafter, as model a) and the filtered DNS, however, is not satisfactory. Moreover, the decorrelation between the filtered DNS and model A is much slower than that of the filtered DNS and model B. Therefore, we conclude that the model A, taking into account the interactions between the subgrid and resolvable scales, is a faithful subgrid model for LES for the range of Reynolds numbers considered.
📜 SIMILAR VOLUMES
In this article, large eddy simulation is used to simulate homogeneous shear ows. The spatial discretization is accomplished by the spectral collocation method and a third-order Runge-Kutta method is used to integrate the time-dependent terms. For the estimation of the subgrid-scale stress tensor, t