## Abstract A twoโdimensional theory of Jackson and Hunt for turbulent flow over a shallow ridge is extended to threeโdimensional topography. The results are compared both with theoretical results for a ridge and with surface wind observations from a nearly circular isolated hill. Agreement between
Airflow over an isolated hill
โ Scribed by R. S. Scorer
- Publisher
- John Wiley and Sons
- Year
- 1956
- Tongue
- English
- Weight
- 282 KB
- Volume
- 82
- Category
- Article
- ISSN
- 0035-9009
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โฆ Synopsis
Abstract
Perturbation theory is used to compute the vertical displacement of a uniform airstream passing over a solitary hill: first for a circular hill, then for a hill of oval section lying across the wind, obliquely to it and along it. The diagrams show contours of the vertical displacement at four different heights above the hill. It is significant that a small but steepโsided oval hill produces almost as much displacement as a larger circular, lessโsteep hill. When inclined obliquely to the airstream the pattern is very asymmetrical, the displacement being greater over the end of the hill that is farther down wind. A hill lying along the wind produces a very small effect.
๐ SIMILAR VOLUMES
## Abstract A twoโdimensional ridge produces a system of lee waves parallel to it, in a suitable airstream. Synthesizing an isolated hill by superposition of ridges inclined at various angles but intersecting in a point, and representing this by an integral, the interference pattern of the leeโwave
In this paper we present data gathered during a weak case of the Helm wind, an example of supercritical airflow, in the vicinity of Cross Fell in Northern England. Airborne measurements have been made using an instrumented glider with simultaneous ground-based measurements both on a hill summit and