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Experiments on wave breaking in stratified flow over obstacles

Published online by Cambridge University Press:  26 April 2006

Ian P. Castro
Affiliation:
Mechanical Engineering Department, University of Surrey, Guildford, Surrey, GU2 5XH, UK
William H. Snyder
Affiliation:
Atmospheric Sciences Modeling Division, Air Resources Laboratory, National Oceanic and Atmospheric Administration, Research Triangle Park, NC 27711, USA On assignment to the Atmospheric Research and Exposure Assessment Laboratory, US Environmental Protection Agency, Research Triangle Park, NC 27711, USA.

Abstract

Towing-tank experiments on linearly stratified flow over three-dimensional obstacles of various shapes are described. Particular emphasis is given to the parameter regimes which lead to wave breaking aloft, the most important of which is the Froude number defined by Fh = U/Nh, where U, N and h are the flow speed, the Brunt–Väisälä frequency and the hill height, respectively. The effects of other parameters, principally K (= NDU, where D is the fluid depth) and the spanwise and longitudinal aspect ratios of the hill, on wave breaking are also demonstrated. It is shown that the Froude-number range over which wave breaking occurs is generally much more restricted than the predictions of linear (hydrostatic) theories would suggest; nonlinear (Long's model) theories are in somewhat closer agreement with experiment. The results also show that a breaking wave aloft can exist separately from a further recirculating region downstream of the hill under the second lee wave, but that under certain circumstances these can interact to form a massive turbulent zone whose height is much greater than h. Previous theories only give estimates for the upper critical Fh, below which breaking occurs; the experiments also reveal lower critical values, below which there is no wave breaking.

Type
Research Article
Copyright
© 1993 Cambridge University Press

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References

Bacmeister, J. T. & Pierrehumbert, R. T. 1988 On high drag states of non-linear stratified flow over an obstacle. J. Atmos. Sci. 45, 6380.Google Scholar
Baines, P. G. 1977 Upstream influence and Long's model in stratified flows. J. Fluid Mech. 82, 147159.Google Scholar
Castro, I. P. 1987 A note on lee-wave structures in stratified flow over three-dimensional ridges. Tellus 39A, 7281.Google Scholar
Castro, I. P. & Snyder, W. H. 1988 Upstream motions in stratified flow. J. Fluid Mech. 187, 487506.Google Scholar
Castro, I. P. & Snyder, W. H. 1990 Obstacle drag and upstream motions in stratified flow. In Stratified Flows (ed. E. J. List & G. H. Jirka), pp. 8498. ASCE.
Castro, I. P., Snyder, W. H. & Baines, P. G. 1990 Obstacle drag in stratified flow. Proc. R. Soc. Lond. A 429, 119140.Google Scholar
Castro, I. P., Snyder, W. H. & Marsh, G. L. 1983 Stratified flow over three-dimensional ridges. J. Fluid Mech. 135, 261282.Google Scholar
Clark, T. L. & Peltier, W. R. 1977 On the evolution and stability of finite amplitude mountain waves. J. Atmos Sci. 34, 17151730.Google Scholar
Crapper, G. D. 1962 Waves in the lee of a mountain with elliptical contours. Phil. Trans. R. Soc. Lond. A 254, 601.Google Scholar
Durran, D. R. 1986 Another look at downslope windstorms. Part I: the development of analogs to supercritical flow in an infinitely deep, continuously stratified fluid. J. Atmos. Sci. 43, 25272543.Google Scholar
Grimshaw, R. H. J. & Yi, Z. 1991 Resonant generation of finite-amplitude waves by the flow of a uniformly stratified fluid over topography. J. Fluid Mech. 229, 603628.Google Scholar
Hanazaki, H. 1989a Drag coefficient and upstream influence in three-dimensional stratified flow of finite depth. Fluid Dyn Res. 4, 317332.Google Scholar
Hanazaki, H. 1989b Upstream advancing columnar disturbances in two-dimensional stratified flow of finite depth. Phys. Fluids A 1, 19761987.Google Scholar
Hunt, J. C. R. & Snyder, W. H. 1980 Experiments on stably and neutrally stratified flow over a model three-dimensional hill. J. Fluid Mech. 96, 671704.Google Scholar
Huppert, H. E. & Miles, J. W. 1969 Lee waves in a stratified flow. Part 3. Semi-elliptical obstacle. J. Fluid Mech. 35, 481496.Google Scholar
Janowitz, G. S. 1981 Stratified flow over a bounded obstacle in a channel of finite depth. J. Fluid Mech. 110, 160171.Google Scholar
Janowitz, G. S. 1984 Upstream disturbances in stratified channel flow. Unpublished Rep., Dept. of Marine, Earth & Atmospheric Sciences, N.C.State Univ., Raleigh, NC 27650.
Lamb, K. G. 1992 Inviscid flow over an obstacle: some numerical simulations. Paper presented at 4th IMA Conf. on Stably Stratified Flows, Guildford.
Lilly, D. K. & Klemp, J. B. 1979 The effects of terrain shape on non-linear hydrostatic mountain waves. J. Fluid Mech. 95, 241.Google Scholar
Long, R. R. 1953 Some aspects of flow of stratified fluids, I: a theoretical investigation. Tellus 5, 4257.Google Scholar
Miles, J. W. & Huppert, H. E. 1969 Lee waves in a stratified flow. Part 4. Perturbation approximations. J. Fluid Mech. 35, 497525.Google Scholar
Paisley, M. F. & Castro, I. P. 1992 Steady and unsteady computations of strongly stratified flow over two-dimensional obstacles, Paper presented at 4th IMA Conf. on Stably Stratified Flows, Guildford.
Rottman, J. W. & Smith, R. B. 1989 A laboratory model of severe downslope winds. Tellus 41A, 401415.Google Scholar
Smith, R. B. 1985 On severe downslope winds. J. Atmos Sci. 42, 25972603.Google Scholar
Smith, R. B. 1989a Moutain-induced stagnation points in hydrostatic flow. Tellus 41A, 270274.Google Scholar
Smith, R. B. 1989b Hydrostatic airflow over mountains. Adv. Geophys. 31, 141.Google Scholar
Smolarkiewicz, P. K. & Rotunno, R. 1989 Low Froude number flow past three-dimensional obstacles. Part I: baroclinically generated lee vortices. J. Atmos. Sci. 46, 11541164.Google Scholar
Snyder, W. H., Thompson, R. S., Eskridge, R. E., Lawson, R. E., Castro, I. P., Lee, J. T., Hunt, J. C. R. & Ogawa, Y. 1985 The structure of strongly stratified flow over hills: dividing streamline concept. J. Fluid Mech. 152, 249288.Google Scholar
Thompson, R. S. & Snyder, W. H. 1976 EPA Fluid Modeling Facility, Proc. Conf. on Environ. Modeling and Simulation, Cincinnati, USEPA Rep. EPA-600/9-76-016, Washington, D.C.
Wong, K. K. & Kao, T. W. 1970 Stratified flow over extended obstacles and its application to topographical effect on vertical wind shear. J. Atmos. Sci. 27, 884889.Google Scholar