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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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书目名称Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields
编辑Albert Gyr,Franz-S. Rys
视频video
丛书名称ERCOFTAC Series
图书封面Titlebook: Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields;  Albert Gyr,Franz-S. Rys Book 1995 Springer Science+Business Me
描述In regions as densely populated as Western Europe, predictionof the ecological implications of pollutant transport are important inorder to minimise damage in the case of accidents, and to evaluate thepossible influence of existing or planned sources. In most cases, suchpredictions depend on high-speed computation. .The present textbook presents a mathematically explicit introductionin eight chapters: 1: An introduction to the basics of fluid dynamicsof the atmosphere and the local events and mesoscale processes. 2: Thetypes of PDEs describing atmospheric flows for limited area models,the problem of appropriate boundary conditions describing thetopographical constraints, and well-posedness. 3: Thermodynamics ofthe atmosphere, dry and wet, its stability, and radiation processes,budgets and the influence of their sum. 4: Scaling and similarity lawsfor stable and convective turbulent atmospheric boundary layers andthe influence of inhomogeneous terrain on the advection and thevertical dispersion, and the method of large eddy simulation. 5:Statistical processes in turbulent dispersion, turbulent diffusion andchemical reactions in fluxes. 6: Theoretical modelling of diffusionand dispers
出版日期Book 1995
关键词Climatology; Inversion; Large Eddy Simulation; Scale; fluid dynamics; fluid mechanics; air pollution and a
版次1
doihttps://doi.org/10.1007/978-94-015-8547-7
isbn_softcover978-90-481-4501-0
isbn_ebook978-94-015-8547-7Series ISSN 1382-4309 Series E-ISSN 2215-1826
issn_series 1382-4309
copyrightSpringer Science+Business Media B.V. 1995
The information of publication is updating

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Boundary Conditions and Treatment of Topography in Limited-Area Models,s of conserved integrals — are conveniently cast into differential form, the hydrodynamical equations. Depending on the application, these equations are altered to a variety of different forms with different mathematical properties and different requirements on initial and/or boundary conditions in
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Thermodynamic and Radiative Processes in the Atmosphere, and thermal characteristics of the atmosphere. Air flow will determine the speed and direction with which a meteorological variable will be transported and dispersed, while the thermal structure of the atmosphere will control the nature of the dispersion through local stability or instability, such
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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 g
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Reflexive Practice for the Times We Live In as the presence of inversion layers which act as a “lid” and strongly inhibit vertical motion. Inversion situations are especially important for air quality problems, as poor dispersion and trapping of pollutants beneath the inversion will inevitably lead to poor local and regional air quality.
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Book 1995amage in the case of accidents, and to evaluate thepossible influence of existing or planned sources. In most cases, suchpredictions depend on high-speed computation. .The present textbook presents a mathematically explicit introductionin eight chapters: 1: An introduction to the basics of fluid dyn
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