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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Similarity Relations, Scaling Laws and Spectral Dynamics,or a series of field observations is not complete when a stack of computer tapes full of numbers is obtained. At that point, the scientist involved faces the task of presenting his or her data in such a way that the results can be understood and employed most easily. Often (not always) this requires

defeatist

總

Diffusion in the Convective Boundary Layer,e is greater than that of the fluid. In this state, thermal energy acquired by fluid in contact with the surface results In a decrease in the density of this fluid; and therefore, in the presence of a gravitational field, potential energy is acquired which puts the fluid system as a whole in a state

CORE

Diffusion in the Stable Boundary Layer,nd extend some of the main theoretical ideas and models that have been found to describe various aspects of turbulent diffusion in the atmospheric boundary 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 t

冬眠

Applications in Air Pollution Modeling, last three chapters was to discuss how this new knowledge of the PBL could be used to develop new and improved diffusion theories and models. Chapters 5 and 6 dealt specifically with diffusion in the convective boundary layer and the stable boundary layer, respectively. Clearly they have pre-empted

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Report from the Panel Discussion,jects, relevant within the context of the course, between the participants and the lecturers. The outcome of this discussion may be valuable to a wider audience. Therefore, it was thought to be useful to include in this book an impression of the questions, comments and remarks expressed during this

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