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Meridional distributions of NO{sub x}, NO{sub y}, and other species in the lower stratosphere and upper troposphere during AASE II

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1029/94GL01897· OSTI ID:57041
; ;  [1];  [2]; ; ;  [3]; ; ;
  1. National Center for Atmospheric Research, Boulder, CO (United States)
  2. Jet Propulsion Lab., Pasadena, CA (United States)
  3. Univ. of California, Irvine, CA (United States)
The meridional distribution of NO{sub x} in the lower stratosphere and upper troposphere is inferred from 10 flights of the NASA DC-8 in the northern winter of 1992, along with like distributions of NO{sub y}, NO{sub x}/NO{sub y}, CO, and C{sub 2}Cl{sub 4}. In the lowest few km of the stratosphere there is little vertical gradient in NO{sub x} over the range of latitudes measured (40{degrees}-90{degrees}N). There is a substantial latitudinal gradient, with 50 pptv above the pole and 120 pptv near 40{degrees}N. In the uppermost few km of the troposphere, background values range from 30 pptv over the pole to 90 pptv near 40{degrees}N. On two occasions higher values, up to 140 pptv in the mean, were seen 2-3 km below the tropopause in association with frontal systems. The meridional distributions of CO and C{sub 2}Cl{sub 4} show the same feature, suggesting that the source of the elevated NO{sub x} is near the earth`s surface. 10 refs., 7 figs.
OSTI ID:
57041
Journal Information:
Geophysical Research Letters, Journal Name: Geophysical Research Letters Journal Issue: 23 Vol. 21; ISSN GPRLAJ; ISSN 0094-8276
Country of Publication:
United States
Language:
English

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