By Michel M. Benarie (Eds.)
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Extra info for Atmospheric Pollution 1980, Proceedings of the 14th International Colloquium, UNESCO Building, Paris,
The average emission rate over the pathway segment is the sum of the components due to uncongested (Q) and congested (Q') flow, as given by: where E' corresponds to an average route speed of 20 mi/h, i is the number of vehicles affected by the backup, L = segment length (m), Lq = backup length (m), and + is the duration (seconds) of the backup. Travel on arterials within the CBD is characterized by interrupted flow and low speeds, and a modal emissions treatment should be used. This is available through an adaptation of EPA's modal model.
The formulation of the equations is outlined as is the numerical finite-difference procedure for solving them. €n particular APT can allowwind speed, surface roughness and heat flux to change as a function of distance downwind and carries no restriction on the initial source height. The code also contains pro- vision for simulating deposition via a source depletion model, but this aspect will not be described in the present paper. An example of these capabilities is given in the form of a prediction of the release of a plume into a stably-stratified atmosphere over open countryside and its subsequent behaviour as it crosses increasingly rougher and hotter surburban, and then urban, terrain.
K . P e t e r s , Proc. 4th Symp. Turbulence, Diffusion, Air P o l l u t i o n , Reno, Nevada, January, 1979, Amer. Meteor. SOC. R. Carmichael, T. Kitada and L . K . P e t e r s , Comp. and Fluids, (1980) in press. C. Y. Yang, S u l f u r dioxide photooxidation r a t e s and aerosol format i o n mechanisms: A smog chamber study. , PB-260-910, 1976. W. B r a d s t r e e t , 66th Ann. APCA Meeting, Chicago, IL, June, 1973. R. D. D i s s . , Univ. of K Y , 1979. O. J. Ranzieri, A c o n s i s t e n t scheme f o r estimating d i f f u s i v i t i e s t o be used i n a i r q u a l i t y models, PB-272-484, 1976.