Urban photochemistry in central Tokyo: 1. Observed and modeled OH and HO2 radical concentrations during the winter and summer of 2004

• Published in: Journal of Geophysical Research: Atmospheres 2007-11, Vol.112 (D21), p.n/a
• Main Authors: Kanaya, Yugo, Cao, Renqiu, Akimoto, Hajime, Fukuda, Masato, Komazaki, Yuichi, Yokouchi, Yoko, Koike, Makoto, Tanimoto, Hiroshi, Takegawa, Nobuyuki, Kondo, Yutaka
• Format: Article
• Language: English
• Subjects: Earth sciences; Earth, ocean, space; Exact sciences and technology; OH radical HO2; radical; Tokyo
• ISSN: 0148-0227; 2156-2202
• DOI: 10.1029/2007JD008670

We used laser‐induced fluorescence to measure the concentrations of OH and HO2 radicals in central Tokyo during two intensive campaigns (IMPACT IV and IMPACT L) in January–February and July–August 2004. The estimated detection limit for the 10‐min data was 1.3 × 105 cm−3 for the nighttime and 5.2 × 105 cm−3 for the daytime. The median values of the daytime peak concentrations of HO2 were 1.1 and 5.7 pptv for the winter and summer periods, respectively, while the values for OH were 1.5 × 106 and 6.3 × 106 cm−3. High HO2 mixing ratios (>50 pptv) were observed on a day in summer when O3 mixing ratios exceeded 100 ppbv. The average nighttime concentrations of HO2 were 0.7 and 2.6 pptv for the winter and summer periods, respectively, while the values for OH were 1.8 × 105 and 3.7 × 105 cm−3. A photochemical box model constrained by ancillary observations was able to reproduce daytime OH concentrations reasonably well for both periods, although daytime HO2 concentrations were underestimated in winter and overestimated in summer. Increasing the wintertime hydrocarbon concentrations in the model led to an increase in daytime HO2 concentrations, thereby showing better agreement with observations; however, the model continued to underestimate HO2 concentrations at high NO mixing ratios. This underestimate was most pronounced in the mornings of both periods and during the daytime in winter. We studied processes that are capable of explaining this discrepancy, including unknown reactions of HNO4 or an unidentified HOx source that is linearly scalable to the NO mixing ratio. The important processes in terms of producing radicals were the olefin + O3 reactions in the nighttime of both periods and during the daytime in winter, the photolysis of carbonyls in the daytime for both periods, and the photolysis of HONO during the daytime in winter (using measured HONO concentrations) and during mornings in summer (using estimated HONO concentrations).