Abstract

Most subgrid-scale (SGS) models for large-eddy simulations (LES) are absolutely dissipative (that is, they remove energy from the large scales at each point in the physical space). The actual SGS stresses, however, may transfer energy to the large scales (backscatter) at a given location. Recent work on the LES of transitional flows [Piomelli et al., Phys. Fluids A 2, 257 (1990)] has shown that failure to account for this phenomenon can cause inaccurate prediction of the growth of the perturbations. Direct numerical simulations of transitional and turbulent channel flow and compressible isotropic turbulence are used to study the backscatter phenomenon. In all flows considered roughly 50% of the grid points were experiencing backscatter when a Fourier cutoff filter was used. The backscatter fraction was less with a Gaussian filter, and intermediate with a box filter in physical space. Moreover, the backscatter and forward scatter contributions to the SGS dissipation were comparable, and each was often much larger than the total SGS dissipation. The SGS dissipation (normalized by total dissipation) increased with filter width almost independently of filter type. The amount of backscatter showed an increasing trend with Reynolds number. In the near-wall region of the channel, events characterized by strong Reynolds shear stress correlated fairly well with areas of high SGS dissipation (both forward and backward). In compressible isotropic turbulence similar results were obtained, independent of fluctuation Mach number.

Keywords

PhysicsTurbulenceDissipationReynolds numberFilter (signal processing)MechanicsBackscatter (email)Large eddy simulationMach numberDissipative systemClassical mechanicsStatistical physicsThermodynamics

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Publication Info

Year
1991
Type
article
Volume
3
Issue
7
Pages
1766-1771
Citations
425
Access
Closed

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Ugo Piomelli, W. Cabot, Parviz Moin et al. (1991). Subgrid-scale backscatter in turbulent and transitional flows. Physics of Fluids A Fluid Dynamics , 3 (7) , 1766-1771. https://doi.org/10.1063/1.857956

Identifiers

DOI
10.1063/1.857956