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Air Pollution Modeling and Its Application XII by G. Cautenet, F. Guillard, B. Marticorena, G. Bergametti, F.

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 shipping and Transformation methods within the jap Mediterranean; G. Kallos, etal.Global and Long-Range Transport: Atmospheric Transport-Chemistry Modeling-Some principles for the long run; P. Builtjes. A version for Airborne Poli-Dispersive Particle shipping and Deposition; M.Galperin, D. Syrakov.ETEX Session: the ecu Tracer test: Experimental effects and knowledge Base; K. Nodop, et al. Intercomparison of 2 Long-Range Lagrangian Particle versions with ETEX Tracer info; F.Desiato, et al.New Developments: fresh 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 evaluate 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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To provide some understanding of the fidelity of the technique, a comparison was made of observed versus satellite-derived insolation values for the period 31 July - 8 August, 1988, using GOES-7 measurements. The observed data were taken from available surface pyranometer archives (National Renewable Energy Laboratory, 1992). Because the GOES sensor measures near-instantaneous values and the pyranometer data are hourly averages, exact agreement cannot be expected. Also, the absolute navigation of the GOES-7 image is of order 10 km.

1980, The response of an atmospheric re/action-transport model to changes in input function, Atmos. , 14:671-679. , G. Diak, and S. Masse, 1980, A simple physical model to estimate incident solar radiation at the surface from GOES satellite data, 1. Appl. , 19: 1005- 1012. Grell, G. , J. Dudhia, and D. R. Stauffer, 1994, A Description of the Fifth-Generation Penn State/NCAR Mesoscale Model (MMS). NCAR Technical Note NCARlTN-398+STR, Nationial Center for Atmospheric Research, Boulder, Colorado.

S. , 1995). Without the assimilation, MM5 overestimates the daytime evaporative flux by 300 Wm- 2 (150%) on both 7 and 8 July. However, use of the satellite data produces a much more realistic time series with an average difference for the 36-h period of less than 40 Wm- 2• DISCLAIMER This paper has been reviewed in accordance with the U. S. Environmental Protection Agency's peer and administrative review policies and approved for presentation and publication. Mention of trade names or commercial products does not constitute endorsements or recommendations.

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