Regime transitions and energetics of sustained stratified shear flows

TL;DR

This study investigates the long-term behavior of stratified shear flows in a laboratory setting, identifying flow regimes and deriving scaling laws for transitions based on experimental data and energy budget analysis.

Contribution

It provides a physical basis and non-dimensional scaling laws for flow regime transitions in sustained stratified shear flows, validated by extensive experiments.

Findings

Four distinct flow regimes identified: laminar, Holmboe waves, intermittent turbulence, vigorous turbulence.

Scaling laws for regime transitions are consistent with experimental data.

Energy budget analysis explains the physical mechanisms behind regime changes.

Abstract

We describe the long-term dynamics of sustained stratified shear flows in the laboratory. The Stratified Inclined Duct (SID) experiment sets up a two-layer exchange flow in an inclined duct connecting two reservoirs containing salt solutions of different densities. This flow is primarily characterised by two non-dimensional parameters: the tilt angle of the duct with respect to the horizontal, $\theta$ (a few degrees at most), and the Reynolds number $Re$, an input parameter based on the density difference driving the flow. The flow can be sustained with constant forcing over arbitrarily long times and exhibits a wealth of dynamical behaviours representative of geophysically-relevant sustained stratified shear flows. Varying $\theta$ and $Re$ leads to four qualitatively different regimes: laminar flow; mostly laminar flow with finite-amplitude, travelling Holmboe waves; spatio-temporally intermittent turbulence with substantial interfacial mixing; and sustained, vigorous interfacial turbulence (Meyer & Linden, J. Fluid Mech., vol. 753, 2014, pp. 242-253). We seek to explain the scaling of the transitions between flow regimes in the two-dimensional plane of input parameters $(\theta, Re)$. We improve upon previous studies of this problem by providing a firm physical basis and non-dimensional scaling laws that are mutually consistent and in good agreement with the empirical transition curves we inferred from 360 experiments spanning $\theta \in [-1^\circ, 6^\circ]$ and $Re \in [300, 5000]$. To do so, we employ state-of-the-art simultaneous volumetric measurements of the density field and the three-component velocity field, and analyse these experimental data using time- and volume-averaged potential and kinetic energy budgets. We show that regime transitions are caused by ...