Atmos. Chem. Phys. Discuss., 6, 6255-6297, 2006
www.atmos-chem-phys-discuss.net/6/6255/2006/
doi:10.5194/acpd-6-6255-2006
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Pronounced signature of arctic surface ozone depletion events after polar sunrise on Δ17O in atmospheric nitrate
S. Morin1, J. Savarino1, S. Bekki2, S. Gong3, and J. W. Bottenheim3
1Laboratoire de Glaciologie et de Géophysique de l’Environnement, Grenoble, France
2Service d’Aéronomie, Institut Pierre Simon Laplace, Paris, France
3Environment Canada, Toronto, Ontario, Canada

Abstract. We report in this paper the first measurements of the isotopic anomaly of oxygen in Arctic atmospheric inorganic nitrate. Data and samples were collected at Alert, Nunavut, Canada (82°30' N, 62°19' W) in spring 2004. Focusing on the polar sunrise period, characterized by the occurrence of severe boundary layer ozone depletion events (ODEs), our data show a significant correlation between the evolution of atmospheric ozone (O3) mixing ratios and Δ17O in nitrate Δ17O(NO3)). This relationship can be expressed as: Δ17O(NO3)/‰=0.15 O3/ (nmol mol−1) + 28.6, with R2=0.70 (n=12), for Δ17O(NO3) ranging between 29 and 34. To quantitatively interpret this relationship, we derive from mechanisms at play in the arctic boundary layer isotopic mass-balance equations, which depend on the concentrations of reactive species and their isotopic characteristics. Changes in the relative importance of O3, RO2 and BrO in the oxidation of NOx during ODEs, and the large isotopic anomalies that O3 and BrO carry, are the driving force for the high variability in the measured Δ17O(NO3). BrONO2 hydrolysis is found to be the major source of nitrate in the arctic boundary layer, in agreement with recent modeling studies. In addition, the isotopic fingerprint of the activity of ozone in a relatively stable compound appears somewhat promising in the perspective of using the isotopic composition of nitrate embedded in polar ice-cores as a paleo-indicator of the atmospheric ozone level that may yield an indirect proxy for the oxidative power of past atmospheres.

Citation: Morin, S., Savarino, J., Bekki, S., Gong, S., and Bottenheim, J. W.: Pronounced signature of arctic surface ozone depletion events after polar sunrise on Δ17O in atmospheric nitrate, Atmos. Chem. Phys. Discuss., 6, 6255-6297, doi:10.5194/acpd-6-6255-2006, 2006.
 
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