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
Structure parameters in the atmospheric surface layer
β Scribed by E. F. Bradley; R. A. Antonia
- Publisher
- John Wiley and Sons
- Year
- 1979
- Tongue
- English
- Weight
- 636 KB
- Volume
- 105
- Category
- Article
- ISSN
- 0035-9009
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β¦ Synopsis
Abstract
The behaviour of structure parameters, relating turbulence properties to other turbulence properties, has been determined from atmospheric surface layer data obtained over both land and ocean. The ratio of momentum flux to turbulence energy is found to decrease significantly as the instability increases. Structure parameters relating heat and moisture fluxes to variances of temperature and humidity fluctuations, respectively, also exhibit a strong stability dependence, under unstable conditions. MoninβObukhov similarity for these parameters seems to be satisfied by only part of the data examined. Neutral values of these parameters are smaller than corresponding values obtained in the laboratory boundary layer. Possible reasons for this difference are discussed.
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