Articles | Volume 16, issue 5
Atmos. Chem. Phys., 16, 2747–2764, 2016
Atmos. Chem. Phys., 16, 2747–2764, 2016

Research article 04 Mar 2016

Research article | 04 Mar 2016

Detailed budget analysis of HONO in central London reveals a missing daytime source

J. D. Lee1,2, L. K. Whalley3,4, D. E. Heard3,4, D. Stone4, R. E. Dunmore2, J. F. Hamilton2, D. E. Young5,a, J. D. Allan5,6, S. Laufs7, and J. Kleffmann7 J. D. Lee et al.
  • 1National Centre for Atmospheric Science, University of York, York, UK
  • 2Department of Chemistry, University of York, York, UK
  • 3National Centre for Atmospheric Science, University of Leeds, Leeds, UK
  • 4School of Chemistry, University of Leeds, Leeds, UK
  • 5School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Oxford Road, Manchester, M13 9PL, UK
  • 6National Centre for Atmospheric Science, University of Manchester, Oxford Road, Manchester, M13 9PL, UK
  • 7Physikalische und Theoretische Chemie/Fakultät Mathematik und Naturwissenschaften, Bergische Universität Wuppertal (BUW), Gaußstr. 20, 42119 Wuppertal, Germany
  • anow at: Department of Environmental Toxicology, University of California, Davis, CA 95616, USA

Abstract. Measurements of HONO were carried out at an urban background site near central London as part of the Clean air for London (ClearfLo) project in summer 2012. Data were collected from 22 July to 18 August 2014, with peak values of up to 1.8 ppbV at night and non-zero values of between 0.2 and 0.6 ppbV seen during the day. A wide range of other gas phase, aerosol, radiation, and meteorological measurements were made concurrently at the same site, allowing a detailed analysis of the chemistry to be carried out. The peak HONO/NOx ratio of 0.04 is seen at  ∼  02:00 UTC, with the presence of a second, daytime, peak in HONO/NOx of similar magnitude to the night-time peak, suggesting a significant secondary daytime HONO source. A photostationary state calculation of HONO involving formation from the reaction of OH and NO and loss from photolysis, reaction with OH, and dry deposition shows a significant underestimation during the day, with calculated values being close to 0, compared to the measurement average of 0.4 ppbV at midday. The addition of further HONO sources from the literature, including dark conversion of NO2 on surfaces, direct emission, photolysis of ortho-substituted nitrophenols, the postulated formation from the reaction of HO2 ×  H2O with NO2, photolysis of adsorbed HNO3 on ground and aerosols, and HONO produced by photosensitized conversion of NO2 on the surface increases the daytime modelled HONO to 0.1 ppbV, still leaving a significant missing daytime source. The missing HONO is plotted against a series of parameters including NO2 and OH reactivity (used as a proxy for organic material), with little correlation seen. Much better correlation is observed with the product of these species with j(NO2), in particular NO2 and the product of NO2 with OH reactivity. This suggests the missing HONO source is in some way related to NO2 and also requires sunlight. Increasing the photosensitized surface conversion rate of NO2 by a factor of 10 to a mean daytime first-order loss of  ∼ 6 × 10−5 s−1 (but which varies as a function of j(NO2)) closes the daytime HONO budget at all times (apart from the late afternoon), suggesting that urban surfaces may enhance this photosensitized source. The effect of the missing HONO to OH radical production is also investigated and it is shown that the model needs to be constrained to measured HONO in order to accurately reproduce the OH radical measurements.

Short summary
This paper presents field measurements of HONO and a range of other gas phase and particulate species from an urban background site in London. The measured daytime HONO cannot be reproduced with a simple box model and thus a significant daytime missing source of HONO is present. We show that this missing source could be responsible for 40 % of the OH radical source and 57 % of the OH initiation; hence its potential importance for atmospheric oxidation and ozone production.
Final-revised paper