Ozone and PAN Formation Inside and Outside of the Berlin Plume – Process Analysis and Numerical Process Simulation |
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| Authors: | U Corsmeier N Kalthoff B Vogel M-U Hammer F Fiedler Ch Kottmeier A Volz-Thomas S Konrad K Glaser B Neininger M Lehning W Jaeschke M Memmesheimer B Rappenglück G Jakobi |
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| Institution: | (1) Institut für Meteorologie und Klimaforschung (IMK), Forschungszentrum Karlsruhe/Universität Karlsruhe, Postfach 3640, D-76021 Karlsruhe, Germany;(2) Institut für Chemie der Belasteten Atmosphäre (ICG2), Forschungszentrum Jülich, Germany;(3) Institut für Verfahrenstechnik und Dampfkesselwesen (IVD), Universität Stuttgart, Germany;(4) MetAir AG, Menzingen, Switzerland;(5) Institut für Schnee- und Lawinenforschung, Davos Dorf, Switzerland;(6) Zentrum für Umweltforschung (ZUF), Universität Frankfurt, Germany;(7) Förderverein des Rheinischen Instituts für Umweltforschung, Universität zu Köln, Germany;(8) Lehrstuhl für Bioklimatologie und Immissionsforschung, Technische Universität München, Germany |
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| Abstract: | During the BERLIOZ field phase on 20 July 1998 a 40 km wide ozone-plume 30 to 70 km north of Berlin in the lee of the city was detected. The ozone mixing ratio inside the plume was app. 15 ppb higher than outside, mainly caused by high ozone precursor emissions in Berlin, resulting in a net chemical ozone production of 6.5 ppb h–1, which overcompensates ozone advection of –3.6 ppb h–1 andturbulent diffusion of –1.1 ppb h–1. That means, although moreozone leaves the control volume far in the lee of Berlin than enters it at the leeside cityborder and although turbulent diffusion causes a loss of ozone in the leeside control volume the chemical production inside the volume leads to a net ozone increase. Using a semi-Lagrangian mass budget method to estimate the net ozone production, 5.0 ppb h–1 are calculated for theplume. This means a fraction of about 20% of ozone in the plume is producedby local emissions, therefore called `home made' by the Berlin emissions. For the same area KAMM/DRAIS simulations using an observation based initialisation, results in a net production rate between 4.0 and 6.5 ppbh–1, while the threefold nested EURAD model gives 6.0 ppbh–1. The process analysis indicates in many cases goodagreement (10% or better) between measurements and simulations not only in the ozone concentrations but also with respect to the physical and chemical processes governing the total change. Remaining differences are caused by different resolution in time and space of the models and measurements as well as by errors in the emission calculation.The upwind-downwind differences in PAN concentrations are partly similar to those of ozone, because in the BERLIOZ case they are governed mainly by photochemical production. While in the stable boundary layer at night and windward of Berlin 0.1 to 0.3 ppb are detected, in the centre of the plume at noon concentrations between 0.75 ppb and 1.0 ppb are measured. The O3/PAN ratio is about 80 to 120 and thus due to the relatively lowPAN concentrations significantly higher than found in previous studies. The low PAN formation on 20 July, was mainly restricted by the moderate nonmethane hydrocarbon levels, whereas high PAN concentrations of 3.0 ppb on 21 July, are caused by local production in the boundary layer and by large scale advection aloft. |
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| Keywords: | city plume ozone formation PAN formation airborne measurements process studies numerical simulations anthropogenic precursor |
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