Short Range Dispersion within a System of Regular Valleys
Recent years have seen the development, by a number of workers, of models describing airflow over real topography. Within the Boundary-layer Research branch of the Meteorological Office, a two-dimensional, incompressible, non-hydrostatic model of flow over complex terrain has recently been tested against measurements of mean wind and turbulence, in neutral stability, in a system of nearly two-dimensional valleys (Mason and King, 1984).
KeywordsComplex Terrain Valley Floor Geostrophic Wind Model Plume Turbulent Dispersion
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