Summertime NOx measurements during the CHABLIS campaign: can source and sink estimates unravel observed diurnal cycles?

• Published in: Atmospheric Chemistry and Physics
• Main Authors: Bauguitte, S. J.-B., Bloss, W. J., Evans, M. J., Salmon, R. A., Anderson, P. S., Jones, A. E., Lee, J. D., Saiz-Lopez, A., Roscoe, H. K., Wolff, E. W., Plane, J. M. C.
• Format: Text
• Language: English
• Published: 2018
• Subjects: Austral; Halley Research Station; Antarc*; Antarctica
• Online Access: https://doi.org/10.5194/acp-12-989-2012; https://www.atmos-chem-phys.net/12/989/2012/

NO x measurements were conducted at the Halley Research Station, coastal Antarctica, during the austral summer period 1 January–10 February 2005. A clear NO x diurnal cycle was observed with minimum concentrations close to instrumental detection limit (5 pptv) measured between 04:00–05:00 GMT. NO x concentrations peaked (24 pptv) between 19:00–20:00 GMT, approximately 5 h after local solar noon. An optimised box model of NO x concentrations based on production from in-snow nitrate photolysis and chemical loss derives a mean noon emission rate of 3.48 × 10 8 molec cm −2 s −1 , assuming a 100 m boundary layer mixing height, and a relatively short NO x lifetime of ~6.4 h. This emission rate compares to directly measured values ranging from 2.1 to 12.6 × 10 8 molec cm −2 s −1 made on 3 days at the end of the study period. Calculations of the maximum rate of NO 2 loss via a variety of conventional HO x and halogen oxidation processes show that the lifetime of NO x is predominantly controlled by halogen processing, namely BrNO 3 and INO 3 gas-phase formation and their subsequent heterogeneous uptake. Furthermore the presence of halogen oxides is shown to significantly perturb NO x concentrations by decreasing the NO/NO 2 ratio. We conclude that in coastal Antarctica, the potential ozone production efficiency of NO x emitted from the snowpack is mitigated by the more rapid NO x loss due to halogen nitrate hydrolysis.