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Titlebook: Atmospheric Turbulence and Air Pollution Modelling; A Course held in The F. T. M. Nieuwstadt,H. Dop Book 1982 D. Reidel Publishing Company,

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期刊全称Atmospheric Turbulence and Air Pollution Modelling
期刊简称A Course held in The
影响因子2023F. T. M. Nieuwstadt,H. Dop
视频video
学科分类Atmospheric and Oceanographic Sciences Library
图书封面Titlebook: Atmospheric Turbulence and Air Pollution Modelling; A Course held in The F. T. M. Nieuwstadt,H. Dop Book 1982 D. Reidel Publishing Company,
影响因子The study of turbulence in the atmosphere has seen considerable progress in the last decade. To put it briefly: boundary-layer meteorology, the branch of atmospheric science that concentrates on turbulence in the lower atmosphere, has moved from the surface layer into the boundary layer itself. The progress has been made on all fronts: theoretical, numerical and observational. On the other hand, air pollution modeling has not seen such a rapid evolution. It has not benefited as much as it should have from the increasing knowledge in the field of atmospheric turbulence. Air pollution modeling is still in many ways based on observations and theories of the surface layer only. This book aims to bring the reader up to date on recent advances in boundary-layer meteorology and to pave the path for applications in air pollution dispersion problems. The text originates from the material presented during a short course on Atmospheric Turbulence and Air Pollution Modeling held in The Hague during September 1981. This course was sponsored and organized by the Royal Netherlands Meteorological Institute, xi xii PREFACE to which both editors are affiliated. The Netherlands Government Ministry of
Pindex Book 1982
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Neutron Transport Theory and Simulationndary layer. Most of the models tend to have a . range of application (which can be more or less specified), but between them they do reveal most of the general features and trends. In some cases they also lead to useful quantitative predictions.
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Experimental Methods of Fusion Neutronicss 5 and 6 dealt specifically with diffusion in the convective boundary layer and the stable boundary layer, respectively. Clearly they have pre-empted much of what I might say, and I will only briefly cover these areas for the sake of completeness.
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Observed Characteristics of the Atmospheric Boundary Layer,he work on the detailed characteristics and diffusive action of atmospheric flow has been concentrated on the surface layer for the obvious reasons of accessibility and practical interest. Relatively little information exists on the rather inaccessible regions above the surface layer, more especially those beyond the reach of tall towers.
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Diffusion in the Stable Boundary Layer,ndary layer. Most of the models tend to have a . range of application (which can be more or less specified), but between them they do reveal most of the general features and trends. In some cases they also lead to useful quantitative predictions.
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