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Markov chain simulations of vertical dispersion from elevated sources into the neutral planetary boundary layer

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Abstract

A Lagrangian statistical-trajectory model based on a Markov chain relation is used to investigate vertical dispersion from elevated sources into the neutral planetary boundary layer. The model is fully two-dimensional, in that both vertical and longitudinal velocity fluctuations, and their correlation, are simulated explicitly. The best observational information currently available is used to characterize the mean and turbulent structure of the neutral boundary layer. In particular, a realistic vertical profile of the Lagrangian integral time scale is proposed, based partly on a review of direct measurements and partly on a comparison of the model predictions with published diffusion data. The model predictions are shown to agree well with a variety of dispersion observations.

The model is used to study vertical diffusion as a function of release height H, friction velocity u* and surface roughness z 0 for downwind distances up to 10 km from the source. The equivalent Gaussian dispersion parameter Σ z is shown to decrease slightly with an increase in H, and to increase with increases in z 0 or u*. It is demonstrated that relationships valid in a field of homogeneous turbulence can be applied to vertical dispersion in the atmosphere if the release occurs above the region of strongest gradients in the mean and turbulent parameters. Scaling in terms of the standard deviation in elevation angle of the wind at the release point leads to a universal curve which provides accurate estimates of Σ z over a wide range of values of H, z 0 and the meteorological parameters.

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  1. Environmental Research Branch, Whiteshell Nuclear Research Establishment, ROE 1L0, Pinawa, Manitoba, Canada

    P. A. Davis

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Issued as AECL-7652.

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Davis, P.A. Markov chain simulations of vertical dispersion from elevated sources into the neutral planetary boundary layer. Boundary-Layer Meteorol 26, 355–376 (1983). https://doi.org/10.1007/BF00119533

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