The buoyancy flux through a section is the integral of velocity times reduced gravity. In a Boussinesq pure plume in a uniform ambient it is conserved.
Ancestors (5)
Incoming links (67)
- Arrested cubic buoyancy profile
- Attraction to pure plume similarity
- Boussinesq point-source plume
- Boussinesq top-hat plume in a stratified ambient
- Conserved momentum flux of a porous thermal plume
- Constant-speed entraining gravity current on a slope
- Displacement-ventilation interface height
- Eddy buoyancy flux
- Filling box model
- Fixed-speed pure-plume merger and flux conservation
- Forced plume
- Jet length
- Jet limit of the top-hat plume model
- Kinematic plume fluxes
- Multiple-plume displacement ventilation
- Neutral buoyancy-flux mode of a pure plume
- Non-Boussinesq top-hat plume equations
- Past exam of the mathematics course of the University of Cambridge / 2001 / iii / Paper 43 / 3 / a / Solution
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- Plume similarity in power-law stratification
- Pure plume
- Sediment resuspension
- Self-similar starting plume
- Starting plume
- Stratified line-plume height scale
- Top-hat plume model
- Turbulent round jet
- Two-sided top-hat line plume
- Vertical turbulent buoyancy flux
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