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Simultaneous in situ measurements of nitrogen dioxide, nitric oxide, and ozone between 20 and 31 km

1986; American Geophysical Union; Volume: 91; Issue: D5 Linguagem: Inglês

10.1029/jd091id05p05421

2156-2202

M. McFarland, B. A. Ridley, M. H. Proffitt, D. L. Albritton, Thomas L. Thompson, W.J. Harrop, R. Winkler, A. L. Schmeltekopf,

Ionosphere and magnetosphere dynamics

Simultaneous in situ measurements of NO, NO 2 , O 3 , and temperature were made from approximately 20 to 31 km in the stratosphere during July, August, and November. Two of the balloon flights were made from Palestine, Texas (32°N), the third from Gimli, Manitoba (50°N). NO was detected using the chemiluminescence technique; NO 2 was photolyzed to NO prior to detection. Both the NO and NO 2 mixing ratios are in good agreement with most other measurements in this altitude region. To within the combined uncertainties the measured NO 2 to NO ratios agree with those calculated assuming photochemical steady state. There is, however, a tendency for the observed ratio to be larger than the calculated ratio at low altitudes near 32°N, but not at 50°N. Refinements to the experiment will be required to elucidate unequivocal discrepancies. From the observation of a temporal increase in the sum of NO and NO 2 while at constant altitude, it is possible to infer the abundance of N 2 O 5 near noon. Further, a lower‐limit estimate of the total odd nitrogen mixing ratio of 16–19 parts per billion by volume near 30 km is made using the observations of NO x , the estimated N 2 O 5 mixing ratio, and previous measurements of HNO 3 .