By Sven-Erik Gryning, Francis A. Schiermeier
Complaints of the Millennium Nato/Ccms foreign Technical assembly on pollution Modeling and its program, held might 15-19 in Boulder, Colorado.
This quantity is the most recent in a chain of complaints courting again to 1971. The booklet addresses the matter of pollution and stories the most recent findings and advancements in pollution modeling, from a really overseas record of members.
Read Online or Download Air Pollution Modeling and its Application XIV (Air Pollution Modeling and Its Application) PDF
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Extra info for Air Pollution Modeling and its Application XIV (Air Pollution Modeling and Its Application)
Example text
But I agree that these developments had a major impact on local modelling. However, should I then also have given attention to aspects as stratosphere-troposphere exchange which have a major impact on continental and global scale modelling? 15 A. ELIASSEN: Isn't it so that the major basic understanding and tools in air pollution modelling were developed before 1980, a period in which you very easily found some basic milestones? After 1980 people have concentrated on filling gaps in the understanding and refining modelling tools.
T. Rao, 1999: Mesoscale 4DDA analysis on meteorological characteristics of high ozone episodes in 1995. New York State Department of Environmental Conservation Report Zurbenko, I. , 1986: The spectral analysis of time series, North-Holland, Amsterdam, Chapter IV, 105-186 32 DISCUSSION B. BORNSTEIN: Your first ‘final conclusion’ [ bullet 1 in the conclusion slide of the presentation: “The use of different modeling systems, different meteorological models, or different grid cell sizes can introduce large uncertainties to the predictions of daily maximum ozone concentrations on individual days”] seems to disagree with your results, in that it seemed to say that the different model systems and configurations yielded different results.
For the comparison between the RAMS3b/UAM-V modeling system and the SMRAQ modeling system, both modeling systems were run with the horizontal grid cell size of 36 km (Figure 1). Details on the setup of the SMRAQ modeling system can be found in SMRAQ (1997). For the simulations studying the effects of meteorology on ozone predictions, the results from the 12-km RAMS3b/UAM-V simulation were compared to 26 ozone predictions obtained when using the MM5 meteorological fields as described in Zhang and Rao (1999) rather than RAMS3b to drive this simulation.
