Brief Report
May 1981

Wind-Induced Mixing in Stratified Fluid

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Publication: Journal of the Hydraulics Division
Volume 107, Issue 5

Abstract

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.

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Journal of the Hydraulics Division
Volume 107Issue 5May 1981
Pages: 632 - 637

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Published in print: May 1981
Published online: Feb 3, 2021

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C. Kranenburg
Sr. Scientific Officer, Lab. of Fluid Mechanics, Dept. of Civ. Engrg., Delft Univ. of Tech., Stevinweg 4, 2628 CN Delft, The Netherlands

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