IMPROVED LINE PARAMETERS FOR OZONE BANDS IN THE 4.8 AND $10 \mu m$ SPECTRAL REGIONS

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1989

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Ohio State University

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In the present work, we report improved line parameters generated for ozone absorption bands in the 4.8 and 10μm spectral regions. These parameters have been obtained by combining the results of recent analyses of room temperature laboratory absorption spectra of natural and 18O. enriched ozone samples recorded at either 0.005 or 0.010cm−1 resolution with the Fourier transform spectrometer operated on Kitt Peak by the National Solar Observatory. All of the parameters for the 4.8 and 10μm bands have been updated as compared to those on the 1986 HITRAN compilation. In the 10μm region, the results reported by Flaud etal.1.2 and Camy-Peyret etal.3 have been used to compute positions, intensities, and lower state energies for the ν1 and ν3 bands of the 16O3,16O15O18O, and 16O18O16O isotopic species. The corresponding parameters for the ν2+ν3ν2,ν1+ν2ν2,2ν3ν3,ν1+ν3ν1, and 2ν1ν3 hot bands of 16O3 were calculated using energy levels derived from studies of the 4.8, 5.7, and 14.3μm spectral regions. The 2ν1ν3 band has been calculated for the first time; it is unexpectedly strong, with numerous lines observable between 1100 and 1250cm−1. In the 4.8μm region, the positions, intensities, and lower state energies of the 2ν1,ν1+ν3, and 2ν3 bands of 16O3 were taken from Ref. 4. Corresponding parameters for the ν2+2ν3ν2,ν1+ν2+ν3ν2, and 2ν1+ν2ν2 hot bands of 16O3 were calculated using energy levels determined from analysis of the 3.6 and 14.3μm spectral regions. For all bands, air-broadening coefficients at 296 K were calculated from a polynomial in J derived by fitting air-broadening measurements of individual lines in the ν1 and ν3 bands of 16O35. Self-broadening coefficients at 296 K were calculated from a similar fit to the measurements reported by Smith et al.5 The new ozone line parameters yield considerable improvement in the accuracy of high resolution atmospheric transmission and emission calculations in 4.8 and 10μm regions. Simulations generated with the new line parameters are compared with the laboratory spectra and 0.003 cm-1 resolution solar occulation spectra of the stratosphere to illustrate the quality of the new line parameters.

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1 J.-M. Flaud et al., J. Mol. Spectrosc. 118, 334-344 (1986). 2 J.-M. Flaud et al., J. Mol. Spectrosc. 124, 209-217 (1987). 3 C. Camy-Peyret et al., J. Mol. Spectrosc. 118, 345-354 (1986). 4 C. P. Rinsland et al., J. Mol. Spectrosc. 130, 204-212 (1988). 5 M. A. H. Smith et al., J. Opt. Soc. Am. B 5, 585-592 (1988). 6 M. A. H. Smith et al., this session.


Author Institution: Atmospheric Sciences Division, NASA Langley Research Center; Department of Physics, College of William and Mary; Laboratoire de Physique Mol'eculaire et Atmosph'erique, Tour 13 Universit'e Pierre and Marie Curie et CNRS; Department of Physics, University of Denver

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