Abstract
This paper presents relations between the mean vertical displacement (\(\bar z\)) of pollutants and their mean horizontal displacement (x\(\bar x\) ) in the atmospheric boundary layer. A modification of the lagrangian similarity theory applied to atmospheric diffusion extended to the atmospheric boundary layer is developed. According to Pasquill and Smith (1983) the similarity theory of Monin-Obukhov applied to atmospheric diffusion states
where ū is the mean wind speed, c depends on stability and K is the vertical material diffusivity. Considering the eddy diffusivity for momentum and the form of the friction velocity introduced by Yokoyama et al.(1979) a form of ū(c\(\bar z\))for the atmospheric boundary layer is developed. Substituting ū(c\(\bar z\)) in Eq.(1), equating K to the heat diffusivity given by Yokoyama et al.(1979) and integrating, the following expressions can be obtained (where z1 is the boundary layer depth, L is the Monin-Obukhov length, θ=\(\bar x\)/z1; α=\(\bar z\)/z1; αo = zo/z1; k=0.41, β=6.9 and γ=0.92): - neutral and stable conditions: (η=z1/L ≥ 0)
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References
Pasquill, F. and Smith, F.B. 1983. Atmospheric Diffusion, Wiley, N.Y. 105.
Yokoyama, 0.; Gamo, M. and Yamamoto, S. 1979. The vertical profiles of the turbulence quantities in the atmospheric boundary layer. J. Met. Soc.of Japan, 57, 3, 264.
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© 1994 Springer Science+Business Media New York
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Venegas, L.E. (1994). Vertical Diffusion Parameter in the Atmospheric Boundary Layer. In: Gryning, SE., Millán, M.M. (eds) Air Pollution Modeling and Its Application X. NATO · Challenges of Modern Society, vol 18. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-1817-4_64
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DOI: https://doi.org/10.1007/978-1-4615-1817-4_64
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