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Analysis of radical propagation efficiency to assess ozone sensitivity to hydrocarbons and NO x : 2. Long‐lived species as indicators of ozone concentration sensitivity
Author(s) -
Tonnesen Gail S.,
Dennis Robin L.
Publication year - 2000
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 - 10.1029/1999jd900372
Subject(s) - sensitivity (control systems) , ozone , environmental science , hydroxyl radical , meteorology , chemistry , radical , physics , organic chemistry , electronic engineering , engineering
We used an analysis of radical propagation efficiency and OH chain length in a simple trajectory model to propose combinations of long‐lived species that distinguish conditions in which O 3 concentration ([O 3 ]) is NO x ‐limited and radical‐limited. We further examined these indicators in a three‐dimensional grid model. We proposed several new indicators including [H 2 O 2 ]/([O 3 ]+[NO 2 ]), [O 3 ]/[NO x ], and a measure using the OH rate constant weighted concentrations of NO 2 and hydrocarbons. Our analysis also supports the use of several indicators previously proposed by other researchers, including [O 3 ]/[HNO 3 ] and [H 2 O 2 ]/[HNO 3 ]. We found that [HCHO]/[NO 2 ] was more useful than the previously proposed [HCHO]/[NO y ]. We found that the indicators easily distinguished extremely NO x ‐limited or extremely radical‐limited regimes but did not reliably distinguish conditions closer to the transition between these two regimes. We propose that a combined analysis using photochemical model simulations and a large set of indicators of both [O 3 ] sensitivity and local odd oxygen production ( P (O x )) sensitivity to VOC and NO x provides the most complete and useful description of [O 3 ] sensitivity. Time series of the indicators, at least from mid‐morning to late afternoon, provide useful information about the evolution of [O 3 ] sensitivity during the day. Values of the indicators change depending on the [O 3 ] level due in part to the effects of miscellaneous OH and HO 2 termination reactions and to the effects of the composition of the HC mixture on P (O x ). Further evaluation of these indicators using modeling studies, measurements, and test cases with NO x or VOC emissions changes are needed to determine how reliably they distinguish NO x ‐and radical‐limited conditions.

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