Abstract
The purpose of this study was to develop a diffusion model for a continuous point source which takes into account the increase of wind speed with height, and to compare this model with short-range diffusion experiments. The main problem was to find a good expression for the vertical diffusion coefficient. It turned out that good agreement between theory and experiment could only be obtained by introducing a settling speed W for the tracer combined with a conventional expression for the vertical diffusion (K(Z) = K 0Z1−p). An empirical relation was found between K 0 and τ vU and between W and bar σ vU2.
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Van Buijtenen, C.J.P., Holland, J. & Van Leeuwen, D. A numerical diffusion model for continuous releases. Boundary-Layer Meteorol 5, 275–283 (1973). https://doi.org/10.1007/BF00155237
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DOI: https://doi.org/10.1007/BF00155237