Abstract
Semiempirical arguments from Roach and Nieuwstadt concerning Richardson numbers Ri, Rf in stably stratified shear layers and boundary layers appear to bypass uncertainties of turbulence closures. Here it is shown that these arguments can be expressed systematically as a Richardson number "balance' condition, derived formally from standard closure models implementing critical Richardson numbers. The range of validity of this procedure, and hence of the semiempirical arguments, is examined for both slow and rapid modes, and their stability analyzed. The rapid mode is stable under any reasonble assumptions, but the slow or balanced mode could be destabilized if a generalized form of the z/L stability parameter decreased with increasing Ri. -from Author
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CITATION STYLE
Derbyshire, S. H. (1994). A “balanced’’ approach to stable boundary layer dynamics.” Journal of the Atmospheric Sciences, 51(23), 3486–3504. https://doi.org/10.1175/1520-0469(1994)051<3486:AATSBL>2.0.CO;2
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