Competing turbulent cascades and eddy-wave interactions in shallow water equilibria

TL;DR

This paper develops a comprehensive statistical mechanics framework for shallow water equations, revealing complex wave-eddy interactions and fluctuations that challenge previous mean-field assumptions, and provides a more consistent theoretical foundation.

Contribution

It derives a full statistical theory consistent with Liouville's theorem, correcting prior approaches and unveiling complex fluctuation phenomena in shallow water equilibria.

Findings

Microscale wave motions cause strong fluctuations and long-range correlations.

The effective model resembles an elastic membrane with nonlinear wave-renormalized tension.

Joint probability distributions are more complex than previously thought.

Abstract

In recent work, Renaud, Venaille, and Bouchet (RVB) revisit the equilibrium statistical mechanics theory of the shallow water equations, within a microcanonical approach, focusing on a more careful treatment of the energy partition between inertial gravity wave and eddy motions in the equilibrium state, and deriving joint probability distributions for the corresponding dynamical degrees of freedom. The authors derive a Liouville theorem that determines the underlying phase space statistical measure, but then, through some physical arguments, actually compute the equilibrium statistics using a measure that \emph{violates} this theorem. Here, using a more convenient, but essentially equivalent, grand canonical approach, the full statistical theory consistent with the Liouville theorem is derived. The results reveal several significant differences from the previous results: (1) The microscale wave motions lead to a strongly fluctuating thermodynamics, including long-ranged correlations, in contrast to the mean-field-like behavior found by RVB. The final effective model is equivalent to that of an elastic membrane with a nonlinear wave-renormalized surface tension. (2) Even when a mean field approximation is made, a rather more complex joint probability distribution is revealed. Alternative physical arguments fully support the consistency of the results. Of course, the true fluid final steady state relies on dissipative processes not included in the shallow water equations, such as wave breaking and viscous effects, but it is argued that the current theory provides a more mathematically consistent starting point for future work aimed at assessing their impacts.