Mixing and entrainment are suppressed in inclined gravity currents
From MaRDI portal
Publication:5229689
DOI10.1017/jfm.2019.430zbMath1419.76284arXiv1808.08980OpenAlexW2954852194WikidataQ109042420 ScholiaQ109042420MaRDI QIDQ5229689
Maarten van Reeuwijk, C. P. Caulfield, Markus Holzner
Publication date: 19 August 2019
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://arxiv.org/abs/1808.08980
Direct numerical and large eddy simulation of turbulence (76F65) Turbulent transport, mixing (76F25) Stratification effects in turbulence (76F45)
Related Items (11)
Experimental properties of continuously forced, shear-driven, stratified turbulence. Part 1. Mean flows, self-organisation, turbulent fractions ⋮ Experimental properties of continuously forced, shear-driven, stratified turbulence. Part 2. Energetics, anisotropy, parameterisation ⋮ Dispersion effects in porous medium gravity currents experiencing local drainage ⋮ Statistical characterisation of turbulence for an unsteady gravity current ⋮ Unified description of turbulent entrainment ⋮ Connecting the time evolution of the turbulence interface to coherent structures ⋮ Goldilocks mixing in oceanic shear-induced turbulent overturns ⋮ Global and local spreading rate estimation in forced plumes ⋮ Lagrangian coherent structures and entrainment near the turbulent/non-turbulent interface of a gravity current ⋮ Development of gravity currents on slopes under different interfacial instability conditions ⋮ Slope dependence of self-similar structure and entrainment in gravity currents
Cites Work
- Unnamed Item
- Unnamed Item
- Symmetry-preserving discretization of turbulent flow.
- Virtual origin correction for lazy turbulent plumes
- Diapycnal diffusivity, turbulent Prandtl number and mixing efficiency in Boussinesq stratified turbulence
- The intermittency boundary in stratified plane Couette flow
- Effects of mean shear on the local turbulent entrainment process
- Two-dimensional density currents in a confined basin
- Turbulent transport of heat and momentum from an infinite rough plane
- Turbulent entrainment in stratified flows
- Note on a paper of John W. Miles
- Ocean Circulation Kinetic Energy: Reservoirs, Sources, and Sinks
- Turbulent gravitational convection from a point source in a non-uniformly stratified environment
- Self-organized criticality of turbulence in strongly stratified mixing layers
- Parameterization of turbulent fluxes and scales using homogeneous sheared stably stratified turbulence simulations
- Available Potential Energy and Exergy in Stratified Fluids
- Scaling analysis and simulation of strongly stratified turbulent flows
- Self-similar mixing in stratified plane Couette flow for varying Prandtl number
- Fractal scaling of the turbulence interface in gravity currents
- Density Stratification, Turbulence, but How Much Mixing?
- The energy cascade in a strongly stratified fluid
- Interfacial Layers Between Regions of Different Turbulence Intensity
- Buoyancy Effects in Fluids
- Contributions to the theory of heat transfer through a laminar boundary layer
- Mass transfer in laminar flow
- On the stability of heterogeneous shear flows
This page was built for publication: Mixing and entrainment are suppressed in inclined gravity currents