By G. Cautenet, F. Guillard, B. Marticorena, G. Bergametti, F. Dulac, J. Edy (auth.), Sven-Erik Gryning, Nadine Chaumerliac (eds.)
Integrated local Modeling: Modeling of a Saharan airborne dirt and dust occasion; G.Cautenet, et al. Temporal and Spatial Scales for delivery and Transformation methods within the japanese Mediterranean; G. Kallos, etal.Global and Long-Range Transport: Atmospheric Transport-Chemistry Modeling-Some rules for the long run; P. Builtjes. A version for Airborne Poli-Dispersive Particle delivery and Deposition; M.Galperin, D. Syrakov.ETEX Session: the ecu Tracer test: Experimental effects and information Base; K. Nodop, et al. Intercomparison of 2 Long-Range Lagrangian Particle types with ETEX Tracer info; F.Desiato, et al.New Developments: contemporary advancements in Closure and Boundary stipulations for Lagrangian Stochastic Dispersion types; W.L.Physick.Accidental Releases: An Operational Real-Time version Chain for Now and Forecasting of Radioactive Atmospheric Releases at the neighborhood Scale; T. Mikkelsen, et al.Model overview and Verificaton: Numerical Simulation of Meteorological stipulations for height pollutants in Paris; B. Carissimo.Poster Sessions: eighty four extra Articles. writer Index. topic Index.
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Additional info for Air Pollution Modeling and Its Application XII
One or two nested grids were usually configured over the areas of interest and mainly over the Greek Peninsula and the Aegean Sea. For specific cases, a very fine nested grid with 2 km horizontal grid resolution was used in an area approximately 200 km x300 km around Athens. The horizontal grid increments selected were found to be adequate for describing all scales of thermal circulations developed in this region. The model was initialized using I x 1 degree ECMWF analysis files available every 6 hours at the standard pressure levels.
The technique requires hourly surface albedos obtained from clear-sky brightness counts. If a single, cloud-free image were available for each hour of daylight, the brightness counts could be obtained directly from them. However, because cloudy skies are so common, a single, cloud-free image is usually not available. Experience has shown that for a given daylight hour images over a period of 20-30 days are needed to obtain a stable minimum brightness count for that hour, especially in the Southeast during summer when cumulus clouds are ubiquitous.
Compute Surface Albedo for Each Pixel - Start of Post· Processing + r-. - - Compute Surface Insolation lor Each Pixel - - - -~ - - -- MclDAS Area File 01 Surface Insolaflon for Cloudy Sky + MclDAS ( Model Domain } - - - . Specifications Map, Grid, and Extract Surface Insola~on Pixels H J Gridded Surface Insolation Values Figure 2. Flow chart of computational procedures for detennining surface insolation. 28 Figure 3. Surface insolation computed from a satellite image for an 80-km grid lor 1800 GMT Julian Day 216, I 98X.
Air Pollution Modeling and Its Application XII by G. Cautenet, F. Guillard, B. Marticorena, G. Bergametti, F. Dulac, J. Edy (auth.), Sven-Erik Gryning, Nadine Chaumerliac (eds.)