Inclined gravity currents filling basins: the impact of peeling detrainment on transport and vertical structure

DOI10.1017/JFM.2017.196zbMath1387.86013OpenAlexW2611729272MaRDI QIDQ5364738

Charlie A. R. Hogg, Herbert E. Huppert, Jorg Imberger, Stuart B. Dalziel

Publication date: 28 September 2017

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

Full work available at URL: https://doi.org/10.1017/jfm.2017.196

zbMATH Keywords

convectiongravity currentsbuoyant boundary layers

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Experimental work for problems pertaining to fluid mechanics (76-05) Free convection (76R10) Computational methods for problems pertaining to geophysics (86-08) Experimental work for problems pertaining to geophysics (86-05)

Related Items (5)

Source and boundary condition effects on unconfined and confined vertically distributed turbulent plumes ⋮ Enhanced ablation of a vertical ice wall due to an external freshwater plume ⋮ Vertically distributed wall sources of buoyancy. Part 2. Unventilated and ventilated confined spaces ⋮ Instability of a dense seepage layer on a sloping boundary ⋮ On the interaction between oncoming internal waves and a dense gravity current in a two-layer stratification

Cites Work

• Unnamed Item
• On the Lambert \(w\) function
• Shear layers driven by turbulent plumes
• Virtual origin correction for lazy turbulent plumes
• Mixing in flows down gentle slopes into stratified environments
• Two-dimensional density currents in a confined basin
• Turbulent gravitational convection from maintained and instantaneous sources
• Turbulent entrainment in stratified flows
• The long-term circulation driven by density currents in a two-layer stratified basin
• Mixing in a density-driven current flowing down a slope in a rotating fluid
• A geophysical-scale model of vertical natural convection boundary layers
• The ventilated filling box containing a vertically distributed source of buoyancy
• Withdrawal of a stratified fluid from a vertical two-dimensional duct
• Mixing regimes for the flow of dense fluid down slopes into stratified environments

This page was built for publication: Inclined gravity currents filling basins: the impact of peeling detrainment on transport and vertical structure