## Abstract Methods of calculating the eddy diffusivity ฮบ are discussed. It is shown that methods which assume that ฮบ can be regarded as independent of the height, even through a shallow layer, lead to erroneous results: in consequence the frequent use in the literature of the approximate equation
THE TEMPERATURE OF THE HIGHEST LAYERS OF THE ATMOSPHERE
โ Scribed by G. D. Robinson
- Book ID
- 112104350
- Publisher
- John Wiley and Sons
- Year
- 1948
- Tongue
- English
- Weight
- 214 KB
- Volume
- 3
- Category
- Article
- ISSN
- 0043-1656
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๐ SIMILAR VOLUMES
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
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