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Vertical Velocity Profiles in Stratified Flows
The Monin-Obukhov analysis is applied to stably stratified, two-dimensional, hydraulically rough, turbulent, fully developed, open-channel flows. The buoyancy flux is expressed as a function of the velocity and density gradients for cases in which the buoyancy flux may vary over the depth. Resulting vertical velocity profile expressions were verified with experimental data collected in a wide laboratory flume with salt-stratified flows. Sidewall effects on stratified flows are significant in narrow flumes and are magnified in highly stratified flows, as noted in a review of previous works.
Vertical Velocity Profiles in Stratified Flows
The Monin-Obukhov analysis is applied to stably stratified, two-dimensional, hydraulically rough, turbulent, fully developed, open-channel flows. The buoyancy flux is expressed as a function of the velocity and density gradients for cases in which the buoyancy flux may vary over the depth. Resulting vertical velocity profile expressions were verified with experimental data collected in a wide laboratory flume with salt-stratified flows. Sidewall effects on stratified flows are significant in narrow flumes and are magnified in highly stratified flows, as noted in a review of previous works.
Vertical Velocity Profiles in Stratified Flows
McCutcheon, Steve C. (author)
Journal of the Hydraulics Division ; 107 ; 973-988
2021-01-01
161981-01-01 pages
Article (Journal)
Electronic Resource
Unknown
Vertical Mixing in Stratified Tidal Flows
| ASCE | 2021
Model for vertical diffusion in stratified flows
| TIBKAT | 1986
Model for vertical diffusion in stratified flows
| UB Braunschweig | 1986
Closure to “Vertical Mixing in Stratified Tidal Flows”
| ASCE | 2021