Abstract
Overall, NO mixing ratios for measurements made beween 0800 and 1600 LT averaged 2.9 ± 0.1 parts per trillion by volume (pptv), where the uncertainties represent 95% confidence limits in the mean. Concentrations were generally highest near the equator: NO mixing ratios obtained between 0800 and 1600 LT averaged 4.0 ± 0.2 pptv in the 5°S-5°N latitude band and 2.1 ± 0.2 pptv in the 5°-15° bands north and south of the equator. In the equatorial band the average diurnal behavior was a steady rise in NO from early morning until local noon, reaching a peak of about 4.5 pptv that remained until late afternoon before beginning a rapid decline. In the 5°-15° bands north and south of the equator the average diurnal curve for NO was flat (within experimental uncertainties) at about 2 pptv from 0800 to 1600. The NO and O3 measured on SAGA 3 correspond to a loss rate of ozone of ~1 parts per billion by volume (ppbv) O3/day in a region where mean surface O3 is 10 ppbv. -from Authors
Original language | English (US) |
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Pages (from-to) | 16,949-16,954 |
Journal | Journal of Geophysical Research |
Volume | 98 |
Issue number | D9 |
DOIs | |
State | Published - 1993 |
All Science Journal Classification (ASJC) codes
- Condensed Matter Physics
- Physical and Theoretical Chemistry
- Polymers and Plastics
- Materials Chemistry