Titlebook: Air Pollution Modeling and Its Application V; C. Wispelaere,Francis A. Schiermeier,Noor V. Gilla Book 1986 Springer Science+Business Media

prodrome

Parameterization of the Atmospheric Boundary Layer for Air Pollution Dispersion ModelsL is turbulence. Turbulent flows have a wide range of length scales. The scales are bounded from above by the geometry of the flow field and from below by molecular effects. The structure of turbulence is determined by the various sources as well as by the imposed length and time scales. The turbule

Binge-Drinking

ECG769

Modeling the Diurnal Variation of Meteorological Variables within the Boundary Layer — Preliminary Cds outlined by two workgroups (Irwin, 1983; Holtslag et al., 1985). Various techniques for assessing the performance of the meteorological processor are being investigated. One such technique is to average the data by hour of day to produce time-height cross sections, depicting the average diurnal p

作繭自縛

Endemic

Atmospheric Diffusion in the Range 20 to 2000 Kilometerseric turbulent diffusion, a finding well supported by atmospheric diffusion observations over a wide range of scales (Gifford, 1977, 1983a; Barr, 1983). The consequences of this result, which have so far not been considered in dealing with diffusion at shorter ranges, become important for longer ran

新鮮

glisten

狂亂

Use of Meteorological Data to Parameterize Statistical Dispersion Modelsist and it is then necessary to predict the ranges, particularly the upper ranges, of potential exposures in the surrounding area. Climatological data from which can be derived estimates of the occurrence frequencies of weather or stability classes, and a wind rose are used for the purpose.

Consensus

contrast-medium