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Spectral calculations in stably stratified turbulence
Kishore Dutta1, Malay K Nandy1
1Department of Physics, Indian Institute of Technology Guwahati, Guwahati 781039, India.
Physical Review. E, Statistical, Nonlinear, and Soft Matter Physics
|January 24, 2015
Summary
This study reveals anisotropic corrections in stably stratified turbulence, showing layered structures due to buoyancy effects. These findings impact understanding of fluid dynamics and atmospheric science.
Area of Science:
- Fluid Dynamics
- Geophysics
- Atmospheric Science
Background:
- Stably stratified turbulence is crucial in geophysical and atmospheric flows.
- Understanding anisotropic effects is key to accurate modeling.
Purpose of the Study:
- To investigate anisotropic corrections in stably stratified turbulence using a perturbative approach.
- To quantify the impact of buoyancy on turbulence correlation functions and spectra.
Main Methods:
- A Leslie-type perturbative treatment was applied to Boussinesq equations.
- Buoyancy terms were treated as perturbations to isotropic background fields.
- Anisotropic corrections to second order were calculated for velocity-velocity, temperature-temperature, and velocity-temperature correlations.
Main Results:
- Prefactors of anisotropic corrections depend on energy flux, scalar flux, Kolmogorov and Batchelor constants, and eddy-damping amplitudes.
- Anisotropic energy and mean-square temperature spectra scale as k(-3).
- Anisotropic buoyancy spectrum scales as k(-7/3).
- Angle-dependent energy density concentrates around the vertical wave vector, indicating layered structures.
Conclusions:
- The perturbative approach successfully quantifies anisotropic effects in stratified turbulence.
- Results highlight the formation of layered structures due to buoyancy.
- Findings provide a basis for improved models of geophysical and atmospheric turbulence.
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