Self-organized criticality of turbulence in strongly stratified mixing layers

TL;DR

This study demonstrates that turbulence in strongly stratified shear flows self-organizes into a critical state with a consistent Richardson number, characterized by scale-invariant avalanches and universal mixing properties, through direct numerical simulations of Holmboe wave instability.

Contribution

It reveals the emergence of self-organized criticality in stratified turbulence, linking flow energetics, mixing, and scale-invariant avalanche dynamics under Holmboe wave instability.

Findings

Self-organized criticality manifests as a critical Richardson number around 1/4.

Avalanche-like motions localize on the density interface, exhibiting scale invariance.

Universal turbulent flux coefficient of approximately 0.2 for Holmboe wave instability flows.

Abstract

Motivated by the importance of stratified shear flows in geophysical and environmental circumstances, we characterize their energetics, mixing and spectral behavior through a series of direct numerical simulations of turbulence generated by Holmboe wave instability (HWI) under various initial conditions. We focus on circumstances where the stratification is sufficiently `strong' so that HWI is the dominant primary instability of the flow. Our numerical findings demonstrate the emergence of self-organised criticality (SOC) that is manifest as an adjustment of an appropriately defined gradient Richardson number, $Ri_g$, associated with the horizontally-averaged mean flow, in such a way that it is continuously attracted towards a critical value of $Ri_g \sim 1/4$. This self-organization occurs through a continuously reinforced localisation of the `scouring' motions (i.e. `avalanches') that are characteristic of the turbulence induced by the break down of Holmboe wave instabilities and are developed on the upper and lower flanks of the sharply localized density interface, embedded within a much more diffuse shear layer. These localised `avalanches' are also found to exhibit the expected scale invariant characteristics. From an energetics perspective, the emergence of SOC is expressed in the form of a long-lived turbulent flow that remains in a `quasi-equilibrium' state for an extended period of time. Most importantly, the irreversible mixing that results from such self-organised behavior appears to be characterized generically by a universal cumulative turbulent flux coefficient of $\Gamma_c \sim 0.2$ only for turbulent flows engendered by Holmboe wave instability. The existence of this self-organised critical state corroborates the original physical arguments associated with self-regulation of stratified turbulent flows as involving a `kind of equilibrium' as described by Turner (1973).