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Airflow over a two-dimensional escarpment. II: Hydrostatic flow

✍ Scribed by R. O. Pitts; T. J. Lyons


Publisher
John Wiley and Sons
Year
1990
Tongue
English
Weight
1003 KB
Volume
116
Category
Article
ISSN
0035-9009

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✦ Synopsis


Abstract

Hydrostatically dominated forced flow over the asymmetric topography of the Darling Scarp, Western Australia, is modelled using a hydrostatic numerical mesoscale model and compared with observations. Simulations reproduce the essential features of wave overturning and the development of a shooting hydraulic flow. This response is dependent on the wind profile but not on the existence of a critical level. the high backsheared environment leads to a high ratio of the Brunt‐VΓ€isΓ€lΓ€ frequency to wind speed throughout the profile, resulting in short wavelengths, high nonlinearity and overturning. With the ratio of the halfwidth of the topography to the boundary‐layer depth being small, the flow fields are shown to be sensitive to the boundary layer.


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