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024 7 _ |a 10.1029/2006JD008172
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024 7 _ |a 0141-8637
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024 7 _ |a 2128/20417
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037 _ _ |a PreJuSER-57779
041 _ _ |a eng
082 _ _ |a 550
084 _ _ |2 WoS
|a Meteorology & Atmospheric Sciences
100 1 _ |a Liu, L.
|b 0
|0 P:(DE-HGF)0
245 _ _ |a A photochemical modelling study of ozone and formaldehyde generation and budget in the Po basin
260 _ _ |c 2007
|a Washington, DC
|b Union
300 _ _ |a D22303
336 7 _ |a Journal Article
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336 7 _ |a article
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440 _ 0 |a Journal of Geophysical Research D: Atmospheres
|x 0148-0227
|0 6393
|v 112
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a In this work, a photochemical dispersion model, CAMx (Comprehensive Air quality Model with eXtensions) was used to simulate a high ozone episode observed in the Po basin during the 2003 FORMAT (Formaldehyde as a Tracer of Oxidation in the Troposphere) campaign. The study focuses on formaldehyde and ozone, and a budget analysis was set up for interpreting the importance of different processes, namely emission, chemistry, transport and deposition, for three different areas (urban, downwind, suburban) around the Milan metropolitan region. In addition, a sensitivity study was carried out based on 11 different VOC emission scenarios. The results of the budget study show that the strongest O-3 production rate (4 ppbv/hour) occurs in the downwind area of the city of Milan, and that accumulated O3 is transported back to Milan city during nighttime. More than 80% of the HCHO concentration over the Milan metropolitan region is secondary, i. e., photochemically produced from other VOCs. The sensitivity study shows that the emissions of isoprene are not, on average, a controlling factor for the peak concentrations of O3 and HCHO over the model domain because of very few oak trees in this region. Although the paraffinic (PAR) emissions are fairly large, a 20% reduction of PAR yields only 1.7% of HCHO reduction and 2.7% reduction of the O3 peak. The largest reduction of O3 levels can be obtained by reduced xylene (XYL) emissions. A 20% reduction of the total anthropogenic VOC emissions leads to 15.5% (20.3 ppbv) reduction of O3 peak levels over the Milan metropolitan region.
536 _ _ |a Atmosphäre und Klima
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700 1 _ |a Andreani-Aksoyoglu, S.
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700 1 _ |a Keller, J.
|b 2
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700 1 _ |a Braathen, G.O.
|b 3
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700 1 _ |a Schultz, M.
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|u FZJ
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700 1 _ |a Prévôt, A.S.H.
|b 5
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700 1 _ |a Isaksen, I. S. A.
|b 6
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773 _ _ |0 PERI:(DE-600)2016800-7
|a 10.1029/2006JD008172
|g Vol. 112, p. D22303
|p D22303
|q 112|t Journal of Geophysical Research
|v 112
|x 0148-0227
|y 2007
|t Journal of geophysical research / Atmospheres
856 7 _ |u http://dx.doi.org/10.1029/2006JD008172
856 4 _ |u https://juser.fz-juelich.de/record/57779/files/2006JD008172.pdf
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913 1 _ |k P22
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914 1 _ |y 2007
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