## Abstract Many recent measurements of verticalβvelocity spectra in the atmospheric boundary layer are combined in order to derive the dependence of the maximum of the logarithmic spectrum, normalized by surface stress, on stability. An empirical equation is suggested which fits the observations a
Variances and spectra of vertical velocity just above the surface layer
β Scribed by H. A. Panofsky; C. Mazzola
- Publisher
- Springer
- Year
- 1971
- Tongue
- English
- Weight
- 309 KB
- Volume
- 2
- Category
- Article
- ISSN
- 0006-8314
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