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Simultaneous measurements of stratospheric HO x , NO x , and Cl x : Comparison with a photochemical model
Author(s) -
Chance K.,
Traub W. A.,
Johnson D. G.,
Jucks K. W.,
Ciarpallini P.,
Stachnik R. A.,
Salawitch R. J.,
Michelsen H. A.
Publication year - 1996
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 - 10.1029/96jd00064
Subject(s) - microwave limb sounder , stratosphere , jet propulsion , analytical chemistry (journal) , diurnal cycle , physics , atmospheric sciences , chemistry , environmental chemistry , thermodynamics
We report simultaneous measurements of the stratospheric concentration profiles of OH, HO 2 , H 2 O 2 , H 2 O, O 3 , HNO 3 , NO 2 , N 2 O, HCl, HOCl, and ClO during a midlatitude balloon flight in 1989. Measurements were made over almost an entire diurnal cycle by the Smithsonian Astrophysical Observatory Far‐Infrared Spectrometer (FIRS‐2) and the Jet Propulsion Laboratory Balloon Microwave Limb Sounder (BMLS). We analyze these measurements using a photochemical model constrained by observations of long‐lived gases. Measured HO x species (OH and HO 2 ) and H 2 O 2 show fair agreement with theory throughout the diurnal cycle. Measurements of HNO 3 are higher than theory near the concentration peak, while the levels of NO 2 are consistent with the model at most altitudes. Measurements of ClO and HOCl are less than predicted concentrations, suggesting a source of HCl in addition to the reaction of Cl with CH 4 . Possibilities for such a source include a minor HCl + O 2 product channel for the reaction of ClO with OH and a minor HCl + O 3 channel for the reaction of ClO with HO 2 .

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