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
Temperature structure in the atmospheric surface layer
โ Scribed by E. F. Bradley; R. A. Antonia; A. J. Chambers
- Publisher
- Springer
- Year
- 1981
- Tongue
- English
- Weight
- 1015 KB
- Volume
- 20
- Category
- Article
- ISSN
- 0006-8314
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โฆ Synopsis
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 production under near-neutral conditions. For moderately unstable conditions, the ratio of production to dissipation is 1.4. The resulting imbalance in the budget is attributed to the inequality between the three components of the dissipation term. The Kolmogorov constant for temperature is found to be about 0.8.
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