Abstract
A simple model of urban mixing height is developed and yields an equation for the height of the inversion h' as a function of distance downwind into the city in the case of non-planar topography. Since many British cities are not situated on a flat terrain the consideration of the effect of topographical features may be of particular importance. -from Author
Original language | English |
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Pages (from-to) | 215-218 |
Number of pages | 4 |
Journal | Journal of Applied Meteorology |
Volume | 19 |
Issue number | 2 |
DOIs | |
Publication status | Published - 1980 |