Open AccessDeviations from ozone photostationary state during the International Consortium for Atmospheric Research on Transport and Transformation 2004 campaign: Use of measurements and photochemical modeling to assess potential causes
Author(s) -
Griffin Robert J.,
Beckman Pieter J.,
Talbot Robert W.,
Sive Barkley C.,
Varner Ruth K.
Publication year - 2007
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2006jd007604
Subject(s) - photostationary state , isoprene , ozone , radical , nitrogen dioxide , chemistry , photochemistry , nox , nitrogen , mixing ratio , atmospheric chemistry , halogen , atmospheric sciences , combustion , catalysis , organic chemistry , photoisomerization , polymer , alkyl , isomerization , copolymer , geology
Nitric oxide (NO) and nitrogen dioxide (NO 2 ) were monitored at the University of New Hampshire Atmospheric Observing Station at Thompson Farm (TF) during the ICARTT campaign of summer 2004. Simultaneous measurement of ozone (O 3 ), temperature, and the photolysis rate of NO 2 ( j NO2 ) allow for assessment of the O 3 photostationary state (Leighton ratio, Φ). Leighton ratios that are significantly greater than unity indicate that peroxy radicals (PO 2 ), halogen monoxides, nitrate radicals, or some unidentified species convert NO to NO 2 in excess of the reaction between NO and O 3 . Deviations from photostationary state occurred regularly at TF (1.0 ≤ Φ ≤ 5.9), particularly during times of low NO x (NO x = NO + NO 2 ). Such deviations were not controlled by dynamics, as indicated by regressions between Φ and several meteorological parameters. Correlation with j NO2 was moderate, indicating that sunlight probably controls nonlinear processes that affect Φ values. Formation of PO 2 likely is dominated by oxidation of biogenic hydrocarbons, particularly isoprene, the emission of which is driven by photosynthetically active radiation. Halogen atoms are believed to form via photolysis of halogenated methane compounds. Nitrate radicals are believed to be insignificant. Higher Φ values are associated with lower mixing ratios of isoprene and chloroiodomethane and lower ratios of NO x to total active nitrogen, indicating that photochemical aging may very well lead to increased Φ values. PO 2 levels calculated using a zero‐dimensional model constrained by measurements from TF can account for 71% of the observed deviations on average. The remainder is assumed to be associated with halogen atoms, most likely iodine, with necessary mixing ratios up to 0.6 or 1.2 pptv, for chlorine and iodine, respectively.