2019
DOI: 10.1017/jfm.2019.192
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Layer formation and relaminarisation in plane Couette flow with spanwise stratification

Abstract: In this paper we investigate the effect of stable stratification on plane Couette flow when gravity is oriented in the spanwise direction. When the flow is turbulent we observe near-wall layering and associated new mean flows in the form of large scale spanwiseflattened streamwise rolls. The layers exhibit the expected buoyancy scaling l z ∼ U/N where U is a typical horizontal velocity scale and N the buoyancy frequency. We associate the new coherent structures with a stratified modification of the well-known … Show more

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Cited by 11 publications
(19 citation statements)
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References 47 publications
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“…Therefore, they validate the scenario built on the resonance between non-viscous internal gravity waves and the TS waves of the Poiseuille flow. Our study on this linear instability of a realistic flow opens new perspectives in the interpretation and understanding of stratified flow characteristics such as the scaling of coherent structures in stratified turbulent shear flows (Chen et al 2016;Lucas, Caulfield & Kerswell 2019), bridging observations to linear or nonlinear instability characteristics.…”
Section: Resultsmentioning
confidence: 76%
“…Therefore, they validate the scenario built on the resonance between non-viscous internal gravity waves and the TS waves of the Poiseuille flow. Our study on this linear instability of a realistic flow opens new perspectives in the interpretation and understanding of stratified flow characteristics such as the scaling of coherent structures in stratified turbulent shear flows (Chen et al 2016;Lucas, Caulfield & Kerswell 2019), bridging observations to linear or nonlinear instability characteristics.…”
Section: Resultsmentioning
confidence: 76%
“…The figure shows that salt-finger convection can distort a linear mean salinity profile into a staircase-like profile in z ∈ [0, 1], particularly when R ρ is relatively small. Although other mechanisms may be involved in the ocean leading to layer formation, merger and migration, including the presence of a diffusive regime (cold fresh water on top of warm salty water) (Timmermans et al 2008;Radko 2016;Yang et al 2022) or stratified shear flow (Oglethorpe, Caulfield & Woods 2013;Lucas, Caulfield & Kerswell 2017;Taylor & Zhou 2017;Lucas, Caulfield & Kerswell 2019), our work suggests that in horizontally extended domains shearing instabilities may disrupt the finger zones that form the S1, S2 and S3 profiles without destroying the associated staircase structure, leading to well-mixed layers of the type observed in the oceans.…”
Section: Dependence On Density Ratiomentioning
confidence: 85%
“…Despite this recent progress in the understanding of stratified ECS, a connection with realistic fully turbulent stratified shear flow remains unresolved (though Lucas et al (2018) arguably see traces of underlying ECS in recent stratified plane Couette DNS results). In part this is due to the Prandtl number; prior stratified ECS studies have only dealt with unit Prandtl numbers (Eaves & Caulfield 2015;Deguchi 2017;Olvera & Kerswell 2017; and full DNS of stratified shear flow turbulence is restricted in the Prandtl numbers it can access by issues of numerical resolution.…”
Section: Introductionmentioning
confidence: 99%