By Robin L. Dennis (auth.), Sven-Erik Gryning, Francis A. Schiermeier (eds.)
Role of Atmospheric types in pollution coverage and AbatementStrategies: Multipollutant Modeling and coverage: Dressing the Emperor and warding off fake Paradigms; R.L. Dennis. Meteorological points of Ozone Episodes in Southern Ontario: A Mesoscale version research; R.S. Tangirala.Integrated nearby Modeling: Meteorological Modeling in Sydney, Australia: Case research of Smog occasion; P.J. Hurley, et al. Lake Breezes and Their influence on Groundlevel Ozone delivery over Southwestern Ontario and Southeastern Michigan; D.M.L. Sills, P.A.Taylor.Global and Longrange Transport: Sulfur Deposition in Asia: An evaluate of the current scenario and destiny situations; G.R.Carmichael, R.L. Arndt. the ecu lengthy diversity Tracer scan (ETEX): initial review of version Intercomparison workout; G.Archer, et al.New Developments: Mesoscale Modeling of Clouds and Aerosol debris; A.I. Flossmann.Accidental Releases: Validation of a mixture of 2 versions for Longrange Tracer Simulations; J.Brandt, et al.Model review and Verification: pollution in Coastal towns; D.G. Steyn.Poster Session: Use of the UB/NMC version for the Simulation of the Lifecycle of Chernobyl Radioactive Cloud; M.Dacic, B. Telenta. seventy four extra articles. Index.
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Additional resources for Air Pollution Modeling and Its Application XI
RAr'AILIDIS: Regarding the eornparison between nurnerieal predietions and the field data, what was the averaging time for the latter ones'? Do we know that these averaging tirnes are suffieient, in view of changing meteorology, possible loeal effeets in the vicinity of the fidd station, ... R. KUNZ: We assurne that the averaging time of 30 minutes, which was used for the observations, is suffieient to filter out loeal effeets. PAI: Did your field stlldy include measurements of speeies besidcs 0 3 and NO x such as VOC and oxielants?
M3 threshold only small differences to the base run could be found from the model results (Figure 4a). The reductions even lead to growing frequencies because of partly NO x determined chemics. m3 threshold (Figure 4b). m3 ozone are exceeded amount to 5,3% ofthe total area-hours on July 27th in the base run they are reduced to 3,7% respectively 4,0% by Scenario 1 and 2. Induding also industrial emission reductions into scenario 1 nearly doubles the effect. As can be seen from Figure 4 effects differ form day to day.
Kuni, C. Schneider2 and T. VögeIe 2 I Laboratory of Heat Transfer and Environmental Engineering, Aristotle University Thessaloniki, 54006 Thessaloniki, Greece 2 Institut für Technische Thermodynamik, Universität Karlsruhe, 76128 Karlsruhe, Germany ABSTRACT The "Heilbronn Ozone Experiment" was performed in the period 23-26 lune 1994 with the intention to investigate if peak ozone concentrations during summer smog periods may be reduced by the aid 01" short term local scale interventions. The measures taken were estimated to lead to reductions of road traffic emissions in the study area by up to 40%.