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Numerico-empirical analyses of atmospheric diffusion theories

Lamb, Robert G. and Chen, Wen H. and Seinfeld, John H. (1975) Numerico-empirical analyses of atmospheric diffusion theories. Journal of the Atmospheric Sciences, 32 (9). pp. 1794-1807. ISSN 0022-4928. doi:10.1175/1520-0469(1975)032<1794:NEAOAD>2.0.CO;2.

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Numerico-empirical expressions for the particle displacement probability density function from which the mean concentration of material in turbulent fluid may be obtained are derived from the numerical planetary boundary layer model of Deardorff. These expressions are then used to compute profiles of the mean, cross-wind-integrated concentration of an inert pollutant issuing from a continuous point source below a stable layer. Profiles are derived for each of two conditions of atmospheric stability: zi/L=0 and –4.5, where zi is the inversion base height and L the Monin-Obukhov length. The resulting concentration profiles [referred to as the numerico-empirical (NE) profiles] are then used in two separate experiments designed to assess the adequacy of conventional atmospheric diffusion formulations. First, the validity of the atmospheric diffusion equation is assessed by determining for each of the two stabilities cited above the profile of vertical eddy diffusivity that produces the closest fit of the mean concentration predicted by the atmospheric diffusion equation with the NE profiles. Second, comparisons are made between the NE profiles and the corresponding concentration distributions predicted by the Gaussian plume formula with Pasquill-Gifford dispersion parameters, and the Gaussian puff equation with McElroy-Pooler travel-time-dependent dispersion parameters.

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Seinfeld, John H.0000-0003-1344-4068
Additional Information:© 1975 American Meteorological Society. Manuscript received June 19, 1974, in final form March 21, 1975. R.G. Lamb is indebted to Dr. James Deardorff of the National Center for Atmospheric Research for making available the data from which the particle statistics reported here were computed and for sponsoring a visit to NCAR in the summer of 1971 where these same calculations were performed. This work was supported in part by the National Science Foundation under Grant ENG71-02486, and in part by funds from the Environmental Protection Agency under Grant 68-02-1237.
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Environmental Protection Agency (EPA)68-02-1237
Issue or Number:9
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Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:12312
Deposited By: Tony Diaz
Deposited On:26 Nov 2008 17:54
Last Modified:08 Nov 2021 22:27

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