Infrared emission spectra obtained during a balloon flight of the Air Force Geophysics Laboratory SCRIBE system by the University of Denver are used to measure stratospheric N2O5 after sunrise over New Mexico (latitude 33°N). This is the first daytime measurement of N2O5. Comparisons with photochemical modeling show consistency between the observed and predicted decline of N2O5 during the morning hours.
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Blatherwick et al. (1989) studied this question.
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