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Airflow over a two-dimensional escarpment. I: Observations

Pitts, R.O. and Lyons, T.J. (1989) Airflow over a two-dimensional escarpment. I: Observations. Quarterly Journal of the Royal Meteorological Society, 115 (488). p. 965.

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Link to Published Version: http://dx.doi.org/10.1002/qj.49711548810
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Abstract

Observations of forced flow over the highly asymmetric topography of the Darling Scarp, Western Australia, are presented. These are typified by shallow surface gradient winds of 10-20 m s-1 with an inherent critical level aloft and a stable layer produced through nocturnal radiational cooling. The observations highlight a topographically induced hydraulic jump, lee waves or vertically propagating hydrostatic waves depending on the upwind stability and wind profile. The vertically propagating waves and hydraulic jump are observed to produce accelerated flow down the escarpment.

Publication Type: Journal Article
Murdoch Affiliation: School of Biological and Environmental Sciences
Publisher: Royal Meteorological Society
Copyright: (c) The Authors
URI: http://researchrepository.murdoch.edu.au/id/eprint/2280
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