Lebedeff and Hameed 1975
Lebedeff, S.A., and S. Hameed, 1975: Steady-state solution of the semi-empirical diffusion equation for area sources. J. Appl. Meteorol., 14, 546-549, doi:10.1175/1520-0450(1975)014<0546:SSSOTS>2.0.CO;2.
Turbulent transport of material emitted from a surface may be described by the steady-state, two-dimensional, semi-empirical diffusion equation. It is shown that, with wind velocity and eddy diffusivity expressed as power functions of the vertical coordinate, this equation can be solved exactly by introducing a similarity variable. The solution gives the vertical distribution of concentration for area sources in terms of the incomplete gamma function. Implications of the solution are discussed.
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Lebedeff, S.A., and Hameed, S.: Steady-state solution of the semi-empirical diffusion equation for area sources, J. Appl. Meteorol., 14, 546-549, doi:10.1175/1520-0450(1975)014<0546:SSSOTS>2.0.CO;2, 1975.
Lebedeff, S.A., and S. Hameed (1975), Steady-state solution of the semi-empirical diffusion equation for area sources, J. Appl. Meteorol., 14, 546-549, doi:10.1175/1520-0450(1975)014<0546:SSSOTS>2.0.CO;2.
Lebedeff, S.A., and S. Hameed, 1975: Steady-state solution of the semi-empirical diffusion equation for area sources. J. Appl. Meteorol., 14, 546-549, doi:10.1175/1520-0450(1975)014<0546:SSSOTS>2.0.CO;2.
Lebedeff, S.A., & Hameed, S. 1975, J. Appl. Meteorol., 14, 546, doi:10.1175/1520-0450(1975)014<0546:SSSOTS>2.0.CO;2.
Lebedeff SA, Hameed S. Steady-state solution of the semi-empirical diffusion equation for area sources, J Appl Meteorol 1975;14:546-549. doi:10.1175/1520-0450(1975)014<0546:SSSOTS>2.0.CO;2.
S.A. Lebedeff, S. Hameed, J. Appl. Meteorol. 14, 546-549, doi:10.1175/1520-0450(1975)014<0546:SSSOTS>2.0.CO;2 (1975).
