By G. Cautenet, F. Guillard, B. Marticorena, G. Bergametti, F. Dulac, J. Edy (auth.), Sven-Erik Gryning, Nadine Chaumerliac (eds.)
Integrated nearby Modeling: Modeling of a Saharan airborne dirt and dust occasion; G.Cautenet, et al. Temporal and Spatial Scales for shipping and Transformation tactics within the jap Mediterranean; G. Kallos, etal.Global and Long-Range Transport: Atmospheric Transport-Chemistry Modeling-Some principles for the longer term; P. Builtjes. A version for Airborne Poli-Dispersive Particle delivery and Deposition; M.Galperin, D. Syrakov.ETEX Session: the eu Tracer test: Experimental effects and knowledge Base; K. Nodop, et al. Intercomparison of 2 Long-Range Lagrangian Particle versions with ETEX Tracer information; 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 review and Verificaton: Numerical Simulation of Meteorological stipulations for top pollutants in Paris; B. Carissimo.Poster Sessions: eighty four extra Articles. writer Index. topic Index.
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Extra resources for Air Pollution Modeling and Its Application XII
The model simulations include 3-D atmospheric and dispersion modeling at various scales simultaneously. Based on the experimental evidence and the model simulations some useful conclusions should be drawn: • The transport of air masses from Europe towards the Eastern Mediterranean occurs during all seasons with the summer to be the most efficient. Most of the transport occurs within the marine PBL. Horizontal advection was found to be more important in the Eastern part of the Mediterranean. This is in contrast to what was found in the Western Mediterranean and the Iberian Peninsula.
S. Environmental Protection Agency under Cooperative Agreement CR822765-0 1-0. REFERENCES Atwater, M. A. and P. S. , 1974, Numerical calculation of the latitudinal variation of solar radiation for an atmosphere of varying opacity, J. Appl. , 13:289-297. Carlson, T. , 1986, Regional scale estimates of surface moisture availability and thermal inertia using remote thennal measurements. , 1:197-246. Carlson, T. , J. K. Dodd, S. G. Benjamin, and J. N. Cooper, 1981, Satellite estimation of the surface energy balance, moisture availability and thennal inertia, 1.
M. , o. , M. Luria 2, M. Peleg 2, A. Wanger2, and M. Uliasz3 ! University of Athens, Department of Applied Physics, Meteorology Laboratory, Panepistimioupolis, PHYS-5, 15784 Athens, Greece 2 The Hebrew University of Jerusalem, School of Applied Science, Jerusalem 91904, Isracl 3 Colorado State University, Department of Atmospheric Science, Fort Collins, Co 80523, USA INTRODUCTION In several studies during the past, the urban plumes have been extensively considered. In these studies, the spatial and temporal scales of episodic conditions have been dcscribed and emphasis was given to the formation and evolution of air pollution episodes within city limits (or in an area covering a few tens of kilometers around the city) and for a time period of one to two days.