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- W1570452926 abstract "Atmospheric turbulence causes plumes to spread horizontally and vertically and fluctuate randomly. The purpose of this chapter is to understand the plume-atmosphere interactions plume rise, plume downwash, and deposition and to be able to predict them. Plume rise is caused by two phenomena, buoyancy and momentum. Most plumes, especially from power generation, are buoyant. They are hotter than the ambient air and their average molar mass is fairly close to that of pure air. Downwash calculations in plume rIse model enhancements (PRIME) follow three steps. First, the size and location of the building wakes are calculated. Next, the deflection of the streamlines is calculated. Third, the interaction between the plume and the wake is calculated. Denser-than-air plumes spread on the surface and remain fairly homogeneous, with a fairly sharp boundary between the plume and the surrounding air, almost as if the plume forms a separate phase." @default.
- W1570452926 created "2016-06-24" @default.
- W1570452926 creator A5058700772 @default.
- W1570452926 date "2013-10-04" @default.
- W1570452926 modified "2023-09-23" @default.
- W1570452926 title "PLUME–ATMOSPHERE INTERACTIONS" @default.
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- W1570452926 doi "https://doi.org/10.1002/9781118723098.ch7" @default.
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