Dispersion of an urban photochemical plume in Phoenix metropolitan area

Air quality simulations were conducted using MM5/CMAQ modeling platform to study the intricacies introduced by photochemical reactions during the dispersion of urban pollution plume of Phoenix metropolis. The simulation days included the sole ozone episode recorded during 1996–2005, which violated t...

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Bibliographic Details
Published inAtmospheric environment (1994) Vol. 80; pp. 152 - 160
Main Authors Lee, Sang-Mi, Fernando, H.J.S.
Format Journal Article
LanguageEnglish
Published Kidlington Elsevier Ltd 01.12.2013
Elsevier
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Summary:Air quality simulations were conducted using MM5/CMAQ modeling platform to study the intricacies introduced by photochemical reactions during the dispersion of urban pollution plume of Phoenix metropolis. The simulation days included the sole ozone episode recorded during 1996–2005, which violated the previous 1-h ozone standard (0.12 ppm). The modeling results suggest that the Phoenix urban plume can be described in terms of “inert passive dispersion” and “chemically active dispersion”. The former is exemplified by the CO distribution and takes the form of a Gaussian-like plume, for which the source is located at the ground level of the urban core or a freeway. The passive dispersion, nevertheless, is directly subjected to heterogeneities of topography and flow patterns, and hence cannot be strictly Gaussian. The case of active dispersion is much more complicated, and leads to a different plume shape, depending on the chemical reactivity of pollutant species. Secondary pollutants such as ozone and its precursors cause the plume core to have its maximum concentration far downwind of the urban area. Chemical species such as VOCs, which are directly emitted from a source as well as transformed by other primary pollutants, form a plume that qualitatively resembles a transition from an inert plume (CO) to a highly reactive plume (NOx). •Dispersion and chemistry of an urban plume were explained using MM5–CMAQ models.•An urban plume can be described in terms of “inert” and “active” dispersion.•The inert dispersion, exemplified by CO, takes the form of a Gaussian-like plume.•Still, it is subjected to heterogeneities of topography and flow patterns.•The active dispersion leads to a different shape, depending on chemical reactivity.
ISSN:1352-2310
1873-2844
DOI:10.1016/j.atmosenv.2013.07.066