Waves drive large-scale 2D flows in rotating turbulence and cause their demise
Sébastien Gomé, Anna Frishman
TL;DR
This study addresses how rotating 3D turbulence sustains large-scale 2D flows despite forcing that excites 3D inertial waves. It combines direct numerical simulations with a quasi-linear wave-mean-flow kinetic framework to show that near-resonant, scale-separated interactions impose a sign-definite helicity conservation for each wave chirality, directing energy into the large-scale 2D condensate. As rotation increases, resonant coupling weakens and 3D–2D energy transfer vanishes in the fast-rotation limit, producing a transition from 2D-dominated to 3D-dominated wave turbulence. The authors derive analytical expressions for the condensate amplitude and the 3D–2D energy transfer as functions of rotation, Reynolds number, and domain geometry, which align with DNS results. Overall, the work elucidates a fundamental mechanism for two-dimensionalization in rotating turbulence and illustrates how wave-bearing nonlinear systems can self-organize into zero-frequency, anisotropic structures.
Abstract
Turbulence follows a few well-known organizational principles, rooted in conservation laws. One such principle states that a system conserving two sign-definite invariants self-organizes into large-scale structures. Ordinary three-dimensional turbulence does not fall within this paradigm. However, when subject to rotation, 3D turbulence is profoundly altered: rotation produces 3D inertial waves, while also sustaining emergent two-dimensional structures and favoring domain-scale flows called condensates. This interplay raises a fundamental question: why and when are 2D flows sustained even when only 3D waves are excited? Using extensive numerical simulations of the rotating 3D Navier-Stokes equations together with a quasi-linear wave-kinetic theory, we show that near-resonant interactions between 3D waves and a large-scale 2D flow impose an additional conservation law: waves must conserve their helicity separately for each helicity sign. This emergent sign-definite invariant constrains the waves to transfer their energy to large-scale 2D motions. However, as rotation increases, resonance conditions become more restrictive and the energy transfer from the waves to the 2D flow progressively vanishes, leading to a transition between distinct classes of turbulence, from 2D-dominated to 3D-dominated wave turbulence. We derive analytical expressions for this 3D-2D energy transfer as a function of rotation, Reynolds number and domain geometry, which show a good agreement with numerical simulations. Together, these results establish a mechanism underlying two-dimensionalization in rotating turbulence, and, more broadly, illustrate how non-linear systems sustaining waves can self-organize into anisotropic, zero-frequency structures.
