Deprecated: $wgMWOAuthSharedUserIDs=false is deprecated, set $wgMWOAuthSharedUserIDs=true, $wgMWOAuthSharedUserSource='local' instead [Called from MediaWiki\HookContainer\HookContainer::run in /var/www/html/w/includes/HookContainer/HookContainer.php at line 135] in /var/www/html/w/includes/Debug/MWDebug.php on line 372
Robust identification of dynamically distinct regions in stratified turbulence - MaRDI portal

Robust identification of dynamically distinct regions in stratified turbulence

From MaRDI portal
Publication:5360527

DOI10.1017/jfm.2016.617zbMath1383.76265OpenAlexW2528243296MaRDI QIDQ5360527

Unnamed Author, S. M. de Bruyn Kops, J. R. Taylor, Hesam Salehipour, C. P. Caulfield

Publication date: 28 September 2017

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

Full work available at URL: https://www.repository.cam.ac.uk/handle/1810/261108




Related Items

Experimental properties of continuously forced, shear-driven, stratified turbulence. Part 1. Mean flows, self-organisation, turbulent fractionsMixing across stable density interfaces in forced stratified turbulenceCharacterization of wind-shear effects on entrainment in a convective boundary layerStratified turbulent mixing in oscillating shear flowsA localized turbulent mixing layer in a uniformly stratified environmentIntermittency and critical mixing in internally heated stratified channel flowA multi-parameter criterion for layer formation in a stratified shear flow using sorted buoyancy coordinatesA data-driven method for modelling dissipation rates in stratified turbulenceScaling of small vortices in stably stratified shear flowsThe effects of stable stratification on the decay of initially isotropic homogeneous turbulenceMixing in forced stratified turbulence and its dependence on large-scale forcingThe influence of far field stratification on shear-induced turbulent mixingGoldilocks mixing in oceanic shear-induced turbulent overturnsDeep learning of mixing by two ‘atoms’ of stratified turbulenceArea of scalar isosurfaces in homogeneous isotropic turbulence as a function of Reynolds and Schmidt numbersBuoyancy-driven exchange flows in inclined ductsThe dynamics of stratified horizontal shear flows at low Péclet numberLayer formation in horizontally forced stratified turbulence: connecting exact coherent structures to linear instabilitiesQuantifying mixing and available potential energy in vertically periodic simulations of stratified flowsExploiting self-organized criticality in strongly stratified turbulenceParameterization of mixing in stratified open channel flowImplications of inertial subrange scaling for stably stratified mixing



Cites Work