Inviscid invariants of flow equations are crucial in determining the direction of the turbulent energy cascade. In this work we investigate a variant of the three-dimensional Navier-Stokes equations that shares exactly the same ideal invariants (energy and helicity) and the same symmetries (under rotations, reflections, and scale transforms) as the original equations. It is demonstrated that the examined system displays a change in the direction of the energy cascade when varying the value of a free parameter which controls the relative weights of the triadic interactions between different helical Fourier modes. The transition from a forward to inverse cascade is shown to occur at a critical point in a discontinuous manner with diverging fluctuations close to criticality. Our work thus supports the observation that purely isotropic and three-dimensional flow configurations can support inverse energy transfer when interactions are altered and that inside all turbulent flows there is a competition among forward and backward transfer mechanisms which might lead to multiple energy-containing turbulent states.

Sahoo, G., Alexakis, A., Biferale, L. (2017). Discontinuous Transition from Direct to Inverse Cascade in Three-Dimensional Turbulence. PHYSICAL REVIEW LETTERS, 118(16), 164501 [10.1103/PhysRevLett.118.164501].

Discontinuous Transition from Direct to Inverse Cascade in Three-Dimensional Turbulence

Biferale L.
2017-01-01

Abstract

Inviscid invariants of flow equations are crucial in determining the direction of the turbulent energy cascade. In this work we investigate a variant of the three-dimensional Navier-Stokes equations that shares exactly the same ideal invariants (energy and helicity) and the same symmetries (under rotations, reflections, and scale transforms) as the original equations. It is demonstrated that the examined system displays a change in the direction of the energy cascade when varying the value of a free parameter which controls the relative weights of the triadic interactions between different helical Fourier modes. The transition from a forward to inverse cascade is shown to occur at a critical point in a discontinuous manner with diverging fluctuations close to criticality. Our work thus supports the observation that purely isotropic and three-dimensional flow configurations can support inverse energy transfer when interactions are altered and that inside all turbulent flows there is a competition among forward and backward transfer mechanisms which might lead to multiple energy-containing turbulent states.
2017
Pubblicato
Rilevanza internazionale
Articolo
Esperti anonimi
Settore FIS/02 - FISICA TEORICA, MODELLI E METODI MATEMATICI
English
Sahoo, G., Alexakis, A., Biferale, L. (2017). Discontinuous Transition from Direct to Inverse Cascade in Three-Dimensional Turbulence. PHYSICAL REVIEW LETTERS, 118(16), 164501 [10.1103/PhysRevLett.118.164501].
Sahoo, G; Alexakis, A; Biferale, L
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2108/214787
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