Research Article
Mar 1978

Vertical Mixing in Stratified Tidal Flows

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Publication: Journal of the Hydraulics Division
Volume 104, Issue 3

Abstract

A set of mixing length functions based on an adaption of the theories of Prandtl, Rossby, Montgomery, and Ellison are presented as a means of calculating the internal shear stresses and vertical flux of solutes in gradually varying turbulent stratified tidal flows. Field observations, made in a straight canalized reach of an estuary, were used to determine the best-fit values of empirical coefficients in generalized relationships between the mixing lengths and gradient Richardson Number. The main purpose of the research was to improve the representation of vertical exchange processes in mathematical models of estuaries.

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Journal of the Hydraulics Division
Volume 104Issue 3March 1978
Pages: 337 - 351

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Published in print: Mar 1978
Published online: Feb 3, 2021

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Nicholas V. M. Odd
Principal Scientific Officer, Estuary Div., Hydr. Research Station, Wallingford, United Kingdom, U.K.
James G. Rodger
Higher Scientific Officer, Estuary Div., Hydr. Research Station, Wallingford, United Kingdom, U.K.

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