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 |
|---|---|
| Pages (from-to) | 215-218 |
| Number of pages | 4 |
| Journal | Journal of Applied Meteorology |
| Volume | 19 |
| Issue number | 2 |
| DOIs | |
| Publication status | Published - 1980 |