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Subgrid scale and backscatter model for magnetohydrodynamic turbulence based on closure theory: theoretical
Ye Zhou1, Oleg Schilling, Sanjoy Ghosh
1Lawrence Livermore National Laboratory, University of California, Livermore, California 94551, USA.
Physical Review. E, Statistical, Nonlinear, and Soft Matter Physics
|September 21, 2002
Summary
This study quantifies eddy viscosity and resistivity in magnetohydrodynamic (MHD) turbulence. The findings offer improved subgrid-scale models for large-eddy simulations of MHD turbulence.
Area of Science:
- Fluid Dynamics
- Plasma Physics
- Magnetohydrodynamics (MHD)
Background:
- Magnetohydrodynamics (MHD) describes fluid dynamics of electrically conducting fluids.
- Turbulence in MHD involves complex interactions between velocity and magnetic fields.
- Subgrid-scale (SGS) modeling is crucial for large-eddy simulations (LES) of turbulent flows.
Purpose of the Study:
- To construct spectral eddy and backscatter viscosity and resistivity for incompressible, 3D, isotropic, nonhelical MHD turbulence.
- To extend existing fluid turbulence closure models to MHD turbulence.
- To provide improved SGS parametrizations for MHD turbulence LES.
Main Methods:
- Utilized the eddy-damped quasinormal Markovian (EDQNM) statistical closure model.
- Extended Leslie and Quarini's methodology for fluid turbulence to MHD.
- Numerically calculated eddy and backscatter coefficients using assumed kinetic and magnetic energy spectra for different Alfvén ratios (r(A)).
Main Results:
- Demonstrated that unresolved scales induce eddy damping and backscatter on resolved scales in MHD turbulence.
- Showed that eddy and backscatter viscosity/resistivity depend on k/k(c) similarly to Navier-Stokes turbulence.
- Quantified these effects for r(A)=1 and r(A)=1/2.
Conclusions:
- The derived eddy and backscatter viscosity and resistivity are essential for accurate MHD turbulence modeling.
- These coefficients can enhance SGS parametrizations in spectral large-eddy simulations of homogeneous MHD turbulence.
- The study provides a foundation for more precise simulations of astrophysical and geophysical MHD phenomena.