Integration of airborne and ground observations of nitryl chloride in the Seoul metropolitan area and the implications on regional oxidation capacity during KORUS-AQ 2016

oleh: D. Jeong, R. Seco, D. Gu, D. Gu, Y. Lee, B. A. Nault, B. A. Nault, C. J. Knote, T. Mcgee, J. T. Sullivan, J. L. Jimenez, J. L. Jimenez, P. Campuzano-Jost, P. Campuzano-Jost, D. R. Blake, D. Sanchez, A. B. Guenther, D. Tanner, L. G. Huey, R. Long, B. E. Anderson, S. R. Hall, K. Ullmann, H. Shin, S. C. Herndon, Y. Lee, D. Kim, J. Ahn, S. Kim

Format: Article
Diterbitkan: Copernicus Publications 2019-10-01

Deskripsi

<p>Nitryl chloride (<span class="inline-formula">ClNO<sub>2</sub></span>) is a radical reservoir species that releases chlorine radicals upon photolysis. An integrated analysis of the impact of <span class="inline-formula">ClNO<sub>2</sub></span> on regional photochemistry in the Seoul metropolitan area (SMA) during the Korea–United States Air Quality Study (KORUS-AQ) 2016 field campaign is presented. Comprehensive multiplatform observations were conducted aboard the NASA DC-8 and at two ground sites (Olympic Park, OP; Taehwa Research Forest, TRF), representing an urbanized area and a forested suburban region, respectively. Positive correlations between daytime <span class="inline-formula">Cl<sub>2</sub></span> and <span class="inline-formula">ClNO<sub>2</sub></span> were observed at both sites, the slope of which was dependent on <span class="inline-formula">O<sub>3</sub></span> levels. The possible mechanisms are explored through box model simulations constrained with observations. The overall diurnal variations in <span class="inline-formula">ClNO<sub>2</sub></span> at both sites appeared similar but the nighttime variations were systematically different. For about half of the observation days at the OP site the level of <span class="inline-formula">ClNO<sub>2</sub></span> increased at sunset but rapidly decreased at around midnight. On the other hand, high levels were observed throughout the night at the TRF site. Significant levels of <span class="inline-formula">ClNO<sub>2</sub></span> were observed at both sites for 4–5&thinsp;h after sunrise. Airborne observations, box model calculations, and back-trajectory analysis consistently show that these high levels of <span class="inline-formula">ClNO<sub>2</sub></span> in the morning are likely from vertical or horizontal transport of air masses from the west. Box model results show that chlorine-radical-initiated chemistry can impact the regional photochemistry by elevating net chemical production rates of ozone by <span class="inline-formula">∼25</span>&thinsp;% in the morning.</p>