On the correlation between turbulent vel
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R. A. Antonia; A. J. Chambers
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Article
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1980
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Springer
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English
โ 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