Isotopic OCS in the troposphere and lower stratosphere determined from high resolution infrared solar absorption spectra

A. Goldman; M. T. Coffey; T. M. Stephen; C. P. Rinsland; W. G. Mankin

doi:10.1364/FTS.1999.FWE12

Fourier Transform Spectroscopy: New Methods and Applications
OSA Technical Digest (Optica Publishing Group, 1999),
paper FWE12
•https://doi.org/10.1364/FTS.1999.FWE12

Isotopic OCS in the troposphere and lower stratosphere determined from high resolution infrared solar absorption spectra

A. Goldman, M. T. Coffey, T. M. Stephen, C. P. Rinsland, and W. G. Mankin

Fourier Transform Spectroscopy 1999

Santa Barbara, California United States
ISBN: 1-55752-598-6

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A. Goldman, M. T. Coffey, T. M. Stephen, C. P. Rinsland, and W. G. Mankin, "Isotopic OCS in the troposphere and lower stratosphere determined from high resolution infrared solar absorption spectra," in Fourier Transform Spectroscopy: New Methods and Applications, OSA Technical Digest (Optica Publishing Group, 1999), paper FWE12.

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Abstract

All previous infrared spectroscopic measurements of atmospheric carbonyl sulfide were limited to v₃ (band center 2062.2 cm⁻¹ transitions of the main isotopomer, ¹⁶O¹²C³²S [Mankin et al., 1979; Zander et al., 1988; Rinsland et al., 1992; Rinsland et al, 1996].

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