Basic Computer Program for the Gaussian Equation for a Point Source

Cota, Harold M.

doi:10.1080/00022470.1984.10465750

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“…For plume rise, a wind integrated average from the physical stack height to the effective stack height is employed, obtained through an iterative process [10]. For dispersion estimates, two options are available: the wind velocity at the effective stack height [15], or an integrated average through the current plume vertical displacement [6,9]. This last approach produces mean transport velocities that are both a function of atmospheric stability and distance downwind from the source.…”

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confidence: 99%