Atmospheric Chemistry and Physics www.atmos-chem-phys.net 1680-7316 1680-7324 7 6 2007 10.5194/acp-7-1683-2007 http://www.atmos-chem-phys.net/7/1683/2007/ http://www.atmos-chem-phys.net/7/1683/2007/acp-7-1683-2007.html http://www.atmos-chem-phys.net/7/1683/2007/acp-7-1683-2007.pdf 1683 1692 2007-03-28 Lightning-produced NO₂ observed by two ground-based UV-visible spectrometers at Vanscoy, Saskatchewan in August 2004 A. Fraser amery@atmosp.physics.utoronto.ca F. Goutail C. A. McLinden S. M. L. Melo K. Strong Department of Physics, University of Toronto, Toronto, Ontario, Canada Service d'Aéronomie du Centre Nationale de la Recherche Scientifique, Verrières le Buisson, France Environment Canada, Downsview, Ontario, Canada Space Science, Canadian Space Agency, Saint-Hubert, Québec, Canada Ground-based measurements of ozone and NO₂ differential slant columns by the SAOZ (Système d'Analyse par Observations Zénithales) and UT-GBS (University of Toronto Ground-Based Spectrometer) instruments during the MANTRA 2004 field campaign are presented herein. During the afternoon of 28 August, a thunderstorm passed over the instruments, which were installed at Vanscoy, Saskatchewan (52° N, 107° W). Enhanced differential slant columns of ozone and NO₂ were observed by both instruments during the storm, with maximum values of two and 25 times the expected clear sky columns, respectively. The enhanced ozone differential slant columns are primarily due to the longer path traversed by the solar radiation caused by multiple scattering inside the thick cloud layer associated with the thunderstorm. The enhanced NO₂ columns are partly attributed to NO_x production by lightning. Two new methods are used to separate the NO₂ enhancements into contributions from the longer path length and production by lightning. Combining the observed excess NO₂ with lightning flash data from the Canadian Lightning Detection Network and Environment Canada Doppler radar measurements, the production of NO₂ molecules per lightning flash is determined. Using these two methods, the best estimate of the production rate is found to be (7.88±2.52)×10²⁶ molecules NO₂/flash from the UT-GBS and (6.81±2.17)×10²⁶ molecules NO₂/flash from SAOZ. These results are consistent with the range of previous estimates reported in the literature. 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