𝔖 Bobbio Scriptorium
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Spectra of temperature derivatives in the atmospheric surface layer

✍ Scribed by R. A. Antonia; A. J. Chambers


Book ID
110608745
Publisher
Springer
Year
1978
Tongue
English
Weight
184 KB
Volume
15
Category
Article
ISSN
0006-8314

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πŸ“œ SIMILAR VOLUMES


Temperature structure in the atmospheric
✍ E. F. Bradley; R. A. Antonia; A. J. Chambers πŸ“‚ Article πŸ“… 1981 πŸ› Springer 🌐 English βš– 1015 KB

Production, transport and dissipation terms in the temperature variance equation have been measured in the atmospheric surface layer. The transport term is, within the experimental uncertainty, negligible. The dissipation term, determined by assuming local isotropy, is approximately equal to product

Temperature structure in the atmospheric
✍ R. A. Antonia; A. J. Chambers; E. F. Bradley πŸ“‚ Article πŸ“… 1981 πŸ› Springer 🌐 English βš– 826 KB

Production, transport and dissipation terms in the mean cube temperature equation have been evaluated from measurements in the atmospheric surface layer under moderately unstable conditions. The transpart term, calcuIated by making use of the quasi-Gaussian approximation, is, on average, comparable

Microscale temperature fluctuations in t
✍ G. A. McBean πŸ“‚ Article πŸ“… 1982 πŸ› Springer 🌐 English βš– 698 KB

Microscale temperature fluctuations were measured at 2 m above a grassy surface. The temperature-derivative spectrum was in general agreement with earlier results but the bump at nondimensional wavenumbers higher than 0.02 was not as pronounced as has been observed. The Obukhov-Corrsin constant for

Spectra and cospectra of turbulence in t
✍ V. Sitaraman πŸ“‚ Article πŸ“… 1970 πŸ› John Wiley and Sons 🌐 English βš– 270 KB

## Abstract Spectra and cospectra of turbulence in the constant‐flux surface layer of the atmosphere are studied with measurements made by rapid response propeller anemometers and a bead thermistor. The results are described in comparison with those obtained at other sites.

On the correlation between turbulent vel
✍ R. A. Antonia; A. J. Chambers πŸ“‚ Article πŸ“… 1980 πŸ› Springer 🌐 English βš– 701 KB

Velocity and temperature derivatives were obtained at a height of 4 m in the atmospheric surface layer above land. With the assumption of local isotropy, these measurements are used to obtain some statistics of the turbulent energy and scalar dissipation fields. These statistics include the variance