This study attempts to determine the scales of turbulence in a high Reynolds number shear flow near which transition to isotropy occurs and the scales for which Taylor's hypothesis is applicable. The flow studied was the wind near height xg = 2 m above a flat land surface. Four hot-wire anemometers
✦ LIBER ✦
The Effect of Scale on the Applicability of Taylor’s Frozen Turbulence Hypothesis in the Atmospheric Boundary Layer
✍ Scribed by Chad W. Higgins; Martin Froidevaux; Valentin Simeonov; Nikki Vercauteren; Caitlin Barry; Marc B. Parlange
- Book ID
- 113062225
- Publisher
- Springer
- Year
- 2012
- Tongue
- English
- Weight
- 845 KB
- Volume
- 143
- Category
- Article
- ISSN
- 0006-8314
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