Abstract
A 2-D meridional model for the chemistry and transport in the troposphere is used to study the seasonal variation of the concentration of organic gases like C2H2, C2H6, C3H8, C6H6, C7H8, CHCl3 and C2 Cl4 at high latitudes. The anthropogenic sources for these species were estimated, and the temporal and latitudinal distribution of OH and 03 was calculated using a complex photochemical reaction system. There is fair agreement between the calculated annual variation and the measured concentrations for C2H2, C2H6, C3H8, C7H8, and C2 Cl4 at Spitsbergen during July 1982 and March/April 1983, with a distinct late winter maximum and summer minimum. For CHC13, the direct anthropogenic source is minor compared to indirect anthropogenic or natural sources. For benzene, emission in car exhaust is important, but other anthropogenic sources are required for the calculations to agree with the measurements. Measured C2H4 and C3H6 concentrations are much higher than the calculated ones based on anthropogenic emissions, and show opposite seasonal trends. This indicates biogenic sources for these compounds.
A buildup of PAN (z300 pptv) is calculated at high latitudes during winter. This makes it the dominant source for N0x as the temperature increases in the spring. N0x is found to be a limiting factor for 03 production at high latitudes during spring.
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Isaksen, I.S.A., Hov, Ø., Penkett, S.A., Semb, A. (1985). Model Analysis of the Measured Concentration of Organic Gases in the Norwegian Arctic. In: Ehhalt, D., Pearman, G., Galbally, I. (eds) Scientific Application of Baseline Observations of Atmospheric Composition (SABOAC). Springer, Dordrecht. https://doi.org/10.1007/978-94-009-3909-7_1
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