New observations of stratospheric N sub 2 O sub 5
Abstract
The unequivocal detection of N2O5 in the stratosphere was reported by Toon et al. based on measurements of the absorption by the N2O5 bands at 1246 and 1720/cm in solar occulation spectra recorded at sunrise near 47 S latitude by the Atmospheric Trace Molecule Spectroscopy (ATMOS) experiment during the Spacelab 3 (SL3) shuttle mission. Additional measurements and analysis of stratospheric N2O5 derived from the ATMOS/SL3 spectra are reported. The primary results are the detection and measurement of N2O5 absorption at sunset in the lower stratosphere, the inversion of a precise (approximately 10 percent) N2O5 sunrise vertical distribution between 25.5 and 37.5 km altitude, and the identification and measurement of absorption by the N2O5 743/cm band at sunrise. Assuming 4.32 x 10(sup -17) and 4.36 x 10(sup -17)/cm/molecule/sq cm respectively for the integrated intensities of the 1246 and 743/cm bands at stratospheric temperatures, retrieved volume mixing ratios in parts per billion by volume (ppbv) at sunrise (47 S latitude) are 1.32 + or - 0.34 at 37.5 km, 1.53 + or - 0.35 at 35.5 km, 1.63 + or - 0.36 at 33.5 km, 1.60 + or - 0.34 at 31.5 km, 1.43 + or - 0.30 at 29.5 km, 1.15more »
- Authors:
- Publication Date:
- Research Org.:
- National Aeronautics and Space Administration, Hampton, VA (USA). Langley Research Center
- OSTI Identifier:
- 6514372
- Report Number(s):
- N-90-26402; NASA-TM-103478; NAS-1.15:103478
- Resource Type:
- Technical Report
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; AIR POLLUTION; MONITORING; NITROGEN OXIDES; STRATOSPHERE; ABSORPTION SPECTRA; DAILY VARIATIONS; MIXING RATIO; PHOTOCHEMICAL REACTIONS; SPECTROSCOPY; CHALCOGENIDES; CHEMICAL REACTIONS; EARTH ATMOSPHERE; NITROGEN COMPOUNDS; OXIDES; OXYGEN COMPOUNDS; POLLUTION; SPECTRA; VARIATIONS; 540120* - Environment, Atmospheric- Chemicals Monitoring & Transport- (1990-)
Citation Formats
Rinsland, C P, Toon, G C, Farmer, C B, Norton, R H, and Namkung, J S. New observations of stratospheric N sub 2 O sub 5. United States: N. p., 1989.
Web.
Rinsland, C P, Toon, G C, Farmer, C B, Norton, R H, & Namkung, J S. New observations of stratospheric N sub 2 O sub 5. United States.
Rinsland, C P, Toon, G C, Farmer, C B, Norton, R H, and Namkung, J S. 1989.
"New observations of stratospheric N sub 2 O sub 5". United States.
@article{osti_6514372,
title = {New observations of stratospheric N sub 2 O sub 5},
author = {Rinsland, C P and Toon, G C and Farmer, C B and Norton, R H and Namkung, J S},
abstractNote = {The unequivocal detection of N2O5 in the stratosphere was reported by Toon et al. based on measurements of the absorption by the N2O5 bands at 1246 and 1720/cm in solar occulation spectra recorded at sunrise near 47 S latitude by the Atmospheric Trace Molecule Spectroscopy (ATMOS) experiment during the Spacelab 3 (SL3) shuttle mission. Additional measurements and analysis of stratospheric N2O5 derived from the ATMOS/SL3 spectra are reported. The primary results are the detection and measurement of N2O5 absorption at sunset in the lower stratosphere, the inversion of a precise (approximately 10 percent) N2O5 sunrise vertical distribution between 25.5 and 37.5 km altitude, and the identification and measurement of absorption by the N2O5 743/cm band at sunrise. Assuming 4.32 x 10(sup -17) and 4.36 x 10(sup -17)/cm/molecule/sq cm respectively for the integrated intensities of the 1246 and 743/cm bands at stratospheric temperatures, retrieved volume mixing ratios in parts per billion by volume (ppbv) at sunrise (47 S latitude) are 1.32 + or - 0.34 at 37.5 km, 1.53 + or - 0.35 at 35.5 km, 1.63 + or - 0.36 at 33.5 km, 1.60 + or - 0.34 at 31.5 km, 1.43 + or - 0.30 at 29.5 km, 1.15 + or - 0.24 at 27.5 km, and 0.73 + or - 0.15 at 25.5 km. Retrieved VMRs in ppbv at sunset (30 N latitude) are 0.13 + or - 0.05 at 29.5 km, 0.14 + or - 0.05 at 27.5 km, and 0.10 + or - 0.04 at 25.5 km. Quoted error limits (1 sigma) include the error in the assumed band intensities (approximately 20 percent). Within the error limits of the measurements, the inferred mixing ratios at sunrise agree with diurnal photochemical model predictions obtained by two groups using current photochemical data. The measured mixing ratios at sunset are lower than the model predictions with differences of about a factor of 2 at 25 km altitude.},
doi = {},
url = {https://www.osti.gov/biblio/6514372},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Sun Jan 01 00:00:00 EST 1989},
month = {Sun Jan 01 00:00:00 EST 1989}
}