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Wind-Induced Mixing in Stratified Fluid
In this note a simple model is offered for mixed-layer deepening caused by wind action at the free surface of a density-stratified fluid. Solar radiation, cooling advection, and Coriolis effects are not considered. To include an aspect of mixing in waters of limited horizontal extent, a steamwise pressure gradient is taken into account.
Wind-Induced Mixing in Stratified Fluid
In this note a simple model is offered for mixed-layer deepening caused by wind action at the free surface of a density-stratified fluid. Solar radiation, cooling advection, and Coriolis effects are not considered. To include an aspect of mixing in waters of limited horizontal extent, a steamwise pressure gradient is taken into account.
Wind-Induced Mixing in Stratified Fluid
Kranenburg, C. (author)
Journal of the Hydraulics Division ; 107 ; 632-637
2021-01-01
61981-01-01 pages
Article (Journal)
Electronic Resource
Unknown
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