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Temperature fluctuations in the atmospheric surface layer over the thermally inhomogeneous underlying surface

✍ Scribed by V. P. Kukharets; H. G. Nalbandyan


Book ID
110147698
Publisher
SP MAIK Nauka/Interperiodica
Year
2006
Tongue
English
Weight
192 KB
Volume
42
Category
Article
ISSN
0001-4338

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πŸ“œ SIMILAR VOLUMES


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

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

Infrared fluctuation hygrometry in the a
✍ M. R. Raupach πŸ“‚ Article πŸ“… 1978 πŸ› John Wiley and Sons 🌐 English βš– 872 KB

## Abstract This paper describes a single‐beam infrared fluctuation hygrometer, operating in the 2.7 ΞΌm water vapour band. By restricting attention to frequencies making up the atmospheric eddy spectrum, a calibration equation for fluctuations is obtained which is independent of moderately stable i