Titlebook: Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields; Albert Gyr,Franz-S. Rys Book 1995 Springer Science+Business Me

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Modelling Diffusion and Dispersion of Pollutants,h scales of atmospheric motion according to:.In spatial extension, the surface layer extends from the ground and up to a few hundred meters in the vertical. It is characterized by approximately constant fluxes of heat and momentum which can be determined by measurements near the surface.

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Inversion layers,ace within so-called atmospheric inversion layers, namely the layers characterized by the increase of the absolute temperature with height. In the course of the diurnal evolution of the atmospheric planetary boundary layer the two most typical examples of the sublayers with the inverse temperature gradient can be observed.

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https://doi.org/10.1007/978-94-015-8547-7Climatology; Inversion; Large Eddy Simulation; Scale; fluid dynamics; fluid mechanics; air pollution and a

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https://doi.org/10.1007/978-3-658-16365-5ance to the distribution of pollutants, are relatively shallow (a few kilometres at most) and are significantly influenced by the nature of the underlying earth’s surface. This chapter is concerned with clarifying the term ‘meso-scale’ and presenting the basic fluid mechanics of meso-scale airflows,

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https://doi.org/10.1007/978-3-658-20005-3djust from their values in the free-atmosphere to the boundary conditions at the earth’s surface. These boundary conditions are the no-slip condition for the velocity and for heat and humidity imposed surface fluxes. The theory of the atmospheric boundary layer should provide us with the vertical pr