## Abstract A twoβdimensional theory of Jackson and Hunt for turbulent flow over a shallow ridge is extended to threeβdimensional 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
Nonlinear shallow fluid flow over an isolated ridge
β Scribed by David D. Houghton; Akira Kasahara
- Publisher
- John Wiley and Sons
- Year
- 1968
- Tongue
- English
- Weight
- 804 KB
- Volume
- 21
- Category
- Article
- ISSN
- 0010-3640
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