Abstract
It is shown that miscellaneous theories for flow over low ridges give results consistent with each other and that these results can be used to quantify certain observed features of the wind profile downwind from an escarpment
| Original language | English |
|---|---|
| Journal | Quarterly Journal of the Royal Meteorological Society |
| Volume | 104 |
| Issue number | 441 |
| Pages (from-to) | 719-728 |
| ISSN | 0035-9009 |
| Publication status | Published - 1978 |
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