By S. Trivikrama Rao, Christian Hogrefe, Gopal Sistla, Shiang-Yuh Wu, Winston Hao (auth.), Sven-Erik Gryning, Ekaterina Batchvarova (eds.)
ISBN-10: 1461368634
ISBN-13: 9781461368632
ISBN-10: 1461541530
ISBN-13: 9781461541530
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Extra info for Air Pollution Modeling and Its Application XIII
Example text
Zlatev. Studying cumulative ozone exposures in Europe during a 7-year period. 1. Geophy. , Vol. 102, No. D 20, October 1997, pp 2391723935. S. G. Zurbenko. Separating different scales ofmotion in time series ofmeteorological variables. Bull. Amer. Meteor. , Vol. 78, No. 10. October 1977, pp 1473-1483. , Lagouvardos, and V. Kotrani. Atmospheric modeling simulations over the Eastern United States with the RAMS3b model for the summer of 1995. Final Report to EPRI, December 1997. W. and Kumar, N. Evaluation of the UAM-V model performance in OTAG simulations Phase I: Summary of performance against surface observations.
I have illustrated how weil the model is reproducing the dynarnical processes influencing the spatial and temporal features embedded in the observations. From my presentation, you can see that there is a very good agreement between the variances of modeled and observed values over the modeling domain. ing results; the model is underestimating the variance in the shorter time scales (intra-day and diurnal) and overestimating at the longer time scales (synoptic and baseline components). Also, I showed results which reveal that the model overstates the effects of local emissions in the near-field and understates the effects of synoptic-scale transport in the far-field.
Under this condition the southwesterly flow at the backside of the high pressure cell favours the transport of ozone and its precursors from the US northeastern seaboard to the SAR. Observations during the 1993 North Atlantic Regional Experiment field campaign indicate that high ozone observed over the Gulf and over the coast ofNova Scotia is generally related to moderate to fast transport from the Boston-New York corridor, typically in the warm sector ahead of an approaching cold front. However, due to the complicated verticallayering structure that dominates the lower atmosphere over the Gulf ofMaine, especially towards the Nova Scotia side, high ozone concentrations are often observed weil above the surface unaccompanied by surface ozone events.
Air Pollution Modeling and Its Application XIII by S. Trivikrama Rao, Christian Hogrefe, Gopal Sistla, Shiang-Yuh Wu, Winston Hao (auth.), Sven-Erik Gryning, Ekaterina Batchvarova (eds.)
by Joseph
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