The concepts of mountain-induced wave drag are applied to the smaller scale problem of the boundary layer over complex terrain. It is found that the Reynolds stress and surface drag caused by surface-generated waves can be at least as large as those conventionally associated with turbulence. Conditi
On mountain wave drag over complex terrain
✍ Scribed by P. R. Bannon; J. A. Yuhas
- Book ID
- 105043811
- Publisher
- Springer
- Year
- 1990
- Tongue
- English
- Weight
- 713 KB
- Volume
- 43
- Category
- Article
- ISSN
- 1436-5065
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