Hostname: page-component-cd9895bd7-jkksz Total loading time: 0 Render date: 2024-12-18T22:24:51.560Z Has data issue: false hasContentIssue false

The development of horizontal boundary layers in stratified flow. Part 1. Non-diffusive flow

Published online by Cambridge University Press:  29 March 2006

R. E. Kelly
Affiliation:
School of Engineering and Applied Science, University of California, Los Angeles, California 90024
L. G. Redekopp
Affiliation:
School of Engineering and Applied Science, University of California, Los Angeles, California 90024 Present address: Department of Aerospace Engineering, University of Colorado, Boulder, Colorado 80302.

Abstract

The development of the boundary layer on the upper surface of a horizontal flat plate in a non-diffusive, stratified flow is described. It is shown that the flow can be characterized by two basic parameters, the Reynolds (RL) and Russell (RuL) numbers, and that, depending on the relative magnitude of these two parameters, three different régimes of flow can be defined. The delineation of these régimes and the description of the flow in each of them is obtained by deriving a uniformly valid first approximation to the Boussinesq equations of motion for a flow contained in the two-dimensional parameter space RuL > 0, RL > 1. The critical stratification for the self-blocking of a horizontal boundary layer is shown to be given by the condition RuL = O(RL½).

Type
Research Article
Copyright
© 1970 Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Graham, E. W. 1966 The two-dimensional flow of an inviscid density-stratified liquid past a slender body. Boeing Scientific Research Laboratories Document DL-72–0550, Flight Sciences Laboratory Report no. 108.Google Scholar
Long, R. R. 1953 Some aspects of the flow of stratified fluids. I. A theoretical investigation. Tellus, 5, 4257.Google Scholar
Long, R. R. 1954 Some aspects of the flow of stratified fluids. II. Experiments with a two-fluid system. Tellus, 6, 97115.Google Scholar
Long, R. R. 1955 Some aspects of the flow of stratified fluids. III. Continuous density gradients. Tellus, 7, 432457.Google Scholar
Long, R. R. 1959 The motion of fluids with density stratification. J. Geophys. Res. 64, 21512163.Google Scholar
Lyra, G. 1943 Theorie der stationären Leewellenstromung in freier Atmosphäre. Z. angew. Math. Mech. 23, 123.Google Scholar
Martin, S. 1966 The slow motion of a finite flat plate in a viscous stratified fluid. The John Hopkins University Technical Report no. 21, ONR series Nonr-4010 (01).Google Scholar
Martin, S. & Long, R. R. 1968 The slow motion of a flat plate in a viscous stratified fluid. J. Fluid Mech. 31, 669688.Google Scholar
Miles, J. W. 1968 Waves and wave drag in stratified flows. Presented at the Twelfth International Congress of Applied Mechanics. Stanford.Google Scholar
Pao, Y.-H. 1968 Laminar flow of a stably stratified fluid past a flat plate. J. Fluid Mech. 34, 795808.Google Scholar
Queney, P., Corby, R., Gerbier, N., Koschmieder, H. & Zierep, J. 1960 The airflow over mountains. World Meteorological Organization, Technical Note no. 34.Google Scholar
Redekopp, L. G. 1969 Horizontal boundary layers in density stratified flows. Ph.D. Thesis, University of California, Los Angeles.
Rosenhead, L. (Ed.) 1963 Laminar boundary layers. Oxford University Press.
Van Dyke, M. D. 1964 Perturbation Methods in Fluid Mechanics. New York: Academic.