Titlebook: Air Pollution Modeling and Its Application II; C. Wispelaere (Operational Director of the Nationa Book 1983 Plenum Press, New York 1983 Eu

Affection

煩躁的女人

https://doi.org/10.1007/978-3-658-14176-9ir pollution modeling.. The SRI model exists in several forms : The simpler form (EURMAP-1) can be used to obtain long-term averages ; the more complicated form (EURMAP-2 ) is used for short-term pollution episodes.

沉思的魚

Nato Challenges of Modern Societyhttp://image.papertrans.cn/a/image/151786.jpg

隨意

咯咯笑

https://doi.org/10.1007/978-3-658-08052-5An air pollution transport model is developed. It will be applied in an area which covers the Netherlands and (parts of) the surrounding countries (500 × 500 km.). Transport is described by

變白

Air Pollutant Reactions in Major Plumes Transported over the North SeaA study is being made of pollutant transport and transformation within a large number of major industrial and urban plumes. The North Sea to the west of The Netherlands was selected as the sampling area for the field experiments conducted during 1979 – 1981.

exacerbate

火車車輪

Chemical Transformation in Plumesnitudes of the resultant pollutant concentrations depend on the chemical composition of a plume and of the ambient air entrained in a plume, the elevation and temperature of a plume, and the meteorological conditions (including solar intensity) experienced by a plume. It is postulated that these tra

occurrence

A Comparison between Chemically Reacting Plume Models and Windtunnel Experimentsfrom NO to NO. has been determined..Based on the results from these experiments and existing field studies, a critical review of chemically reacting plume models has been carried out..It is shown that in principle these models should take into account the effect of inhomogeneous mixing and the corre

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Solutions to the Equation for Surface Depletion of a Gaussian Plume = v. C(x,y,z.), at a given point in computed as the deposition velocity v. times the pollutant concentration, C(x,y,z.), at a particular reference height z. ; however, in Horst’s model C(x,y,z) is the concentration due to the initial, unabsorbed plume minus the sum of concentration deficits due to