(NPPs) are based on Gaussian plume models or on the use of a convection–diffusion
equation. Such methods, which do not involve solving the flow problem, are useful in the
atmospheric mesoscale, of the order of 2–2000km from the NPP. However, they do not
account for the turbulence generated by the interaction of the wind with obstacles and with
the released material stream, which are the dominant factors in the local scale, of the order …