The culmination of an inverse cascade: mean flow and fluctuations
Anna Frishman

TL;DR
This paper reviews and extends a theory explaining how large-scale coherent structures in 2D turbulence are sustained, emphasizing the role of momentum flux and mean shear, supported by simulations and symmetry considerations.
Contribution
It extends the existing theory to show the momentum flux relation holds for both isotropic and anisotropic forcing, regardless of dissipation mechanisms, and discusses its applicability and statistical properties.
Findings
Momentum flux is proportional to inverse shear, valid for various forcing types.
The theory's predictions align with simulation observations.
Symmetry considerations determine the proportionality constant.
Abstract
Two dimensional turbulence has a remarkable tendency to self-organize into large, coherent structures, forming a mean flow. The purpose of this paper is to elucidate how these structures are sustained, and what determines them and the fluctuations around them. A recent theory for the mean flow will be reviewed. The theory assumes turbulence is excited by a forcing supported on small scales, and uses a linear shear model to relate the turbulent momentum flux to the mean shear rate. Extending the theory, it will be shown here that the relation between the momentum flux and mean shear is valid, and the momentum flux is non-zero, for both an isotropic and an anisotropic forcing, independent of the dissipation mechanism at small scales. This conclusion requires taking into account that the linear shear model is an approximation to the real system. The proportionality between the momentum…
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Taxonomy
TopicsFluid Dynamics and Turbulent Flows · Advanced Thermodynamics and Statistical Mechanics
