Abstract
Dispersion in the atmospheric boundary layer (ABL) is a random process caused by the stochastic nature of turbulence. As a result, the fluctuating concentration observed downwind of a source is typically of the same order as the ensemble-mean concentration 〈c〉; the fluctuation is characterized by its root-mean-square value σ c ,. This paper discusses the nature of the fluctuations—σ c and the probability distribution of concentration—as observed in laboratory and field experiments and predicted by models. The focus is on point-source plumes in the ABL. Models for σ c , range from simple methods useful in applications to more research oriented approaches. The first group includes Gifford’s (1959) meandering plume model and ensemble-closure approaches. The research models include large-eddy simulations and Lagrangian stochastic models, which offer promise for obtaining fundamental information about the behavior of the fluctuations; these models have been corroborated in part by wind-tunnel measurements.
The National Center for Atmospheric Research is sponsored by the National Science Foundation.
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© 1995 Springer Science+Business Media Dordrecht
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Weil, J.C. (1995). Concentration Fluctuations in Plumes: Observations and Models. In: Cermak, J.E., Davenport, A.G., Plate, E.J., Viegas, D.X. (eds) Wind Climate in Cities. NATO ASI Series, vol 277. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-3686-2_21
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DOI: https://doi.org/10.1007/978-94-017-3686-2_21
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