Abstract
Observations of flow over complex terrain taken at Risø during June–July 1978 and numerical studies confirm earlier findings that small variations in surface elevation have significant effects on mean wind profiles. Measured shear stresses in the nonequilibrium region of the flow are consistent with theory but quite different from those obtained assuming simple flux-profile relationships. These findings imply that flux-profile relationships can be quite complicated over other than simple homogeneous terrain.
| Original language | English |
|---|---|
| Journal | Boundary-Layer Meteorology |
| Volume | 19 |
| Issue number | 3 |
| Pages (from-to) | 303-313 |
| ISSN | 0006-8314 |
| DOIs | |
| Publication status | Published - 1980 |
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