Boundary-Layer Meteorology

, Volume 23, Issue 1, pp 17–46

On the application of a model of boundary-layer flow over low hills to real terrain

Authors

  • John L. Walmsley
    • Boundary-Layer Research DivisionAtmospheric Environment Service
  • J. R. Salmon
    • Boundary-Layer Research DivisionAtmospheric Environment Service
  • P. A. Taylor
    • Boundary-Layer Research DivisionAtmospheric Environment Service
Article

DOI: 10.1007/BF00116110

Cite this article as:
Walmsley, J.L., Salmon, J.R. & Taylor, P.A. Boundary-Layer Meteorol (1982) 23: 17. doi:10.1007/BF00116110

Abstract

Attempts to apply a computer model (Walmsley et al., 1980) to neutrally-stratified, boundary-layer flow over an isolated hill of moderate slope (Kettles Hill, Alberta) lead to velocity perturbation fields which probably overemphasize the impact of small-scale topographic features. Some numerical smoothing of the digitized terrain input field is found to be helpful in reducing this effect, although such a procedure is somewhat arbitrary. An extension of the original theory results in an improved representation of the effect of small-scale terrain components. These modifications are described and some results of an application of the extended model to Kettles Hill are presented.

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Copyright information

© D. Reidel Publishing Co 1982