Microwave and Infrared Investigations of N2O5

Gerald T. Fraser; J.L. Domenech; J.-U. Grabow; A M. Andrews; K.K. Irikura; R.D. Suenram; F.J. Lovas; A. R. Hight Walker; W.J. Lafferty

doi:10.1364/ORSA.1997.OFA.3

Optical Remote Sensing of the Atmosphere
Technical Digest Series (Optica Publishing Group, 1997),
paper OFA.3
•https://doi.org/10.1364/ORSA.1997.OFA.3

Microwave and Infrared Investigations of N₂O₅

Gerald T. Fraser, J.L. Domenech, J.-U. Grabow, A M. Andrews, K.K. Irikura, R.D. Suenram, F.J. Lovas, A. R. Hight Walker, and W.J. Lafferty

Optical Remote Sensing of the Atmosphere 1997

Santa Fe, New Mexico United States
10–14 February 1997
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Ground Based Trace Species Detection: I (OFA)

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G. T. Fraser, J. L. Domenech, J. -. Grabow, A. M. Andrews, K. K. Irikura, R. D. Suenram, F. J. Lovas, A. R. Hight Walker, and W. J. Lafferty, "Microwave and Infrared Investigations of N2O5," in Optical Remote Sensing of the Atmosphere, Technical Digest Series (Optica Publishing Group, 1997), paper OFA.3.

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Abstract

Dinitrogen pentoxide (N₂O₅) is an important night-time reservoir for NO₂ and NO₃ in the atmosphere. Toon et al.¹ first observed N₂O₅ in the atmosphere in infrared spectra recorded at sunrise by the Atmospheric Trace Molecule Experiment aboard Spacelab 3. Their results have motivated renewed interest in laboratory investigations of N₂O₅ to obtain accurate intensity data for modeling the atmospheric spectra^2-5. Also, ab initio electronic structural calculations have been undertaken to estimate integrated infrared band intensities to compare with the experimental results⁶.

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