Cavity ring-down spectroscopy of CO near = 2.06 m: Accurate transition intensities for the Orbiting Carbon Observatory-2 (OCO-2) "strong band"
arXiv:2002.09584 · doi:10.1016/j.jqsrt.2020.107104
Abstract
The = 2.06 m absorption band of CO is widely used for the remote sensing of atmospheric carbon dioxide, making it relevant to many important top-down measurements of carbon flux. The forward models used in the retrieval algorithms employed in these measurements require increasingly accurate line intensity and line shape data from which absorption cross-sections can be computed. To overcome accuracy limitations of existing line lists, we used frequency-stabilized cavity ring-down spectroscopy to measure 39 transitions in the CO absorption band. The line intensities were measured with an estimated relative combined standard uncertainty of = 0.08 %. We predict the -dependence of the measured intensities using two theoretical modesl: a one-dimensional spectroscopic model with Herman-Wallis rotation-vibration corrections, and a line-by-line ab initio dipole moment surface model [Zak et al. JQSRT 2016;177:31-42]. For the second approach, we fit only a single factor to rescale the theoretical integrated band intensity to be consistent with the measured intensities. We find that the latter approach yields an equally adequate representation of the fitted -dependent intensity data and provides the most physically general representation of the results. Our recommended value for the integrated band intensity equal to 7.18310 cm molecule 610 cm molecule is based on the rescaled ab initio model and corresponds to a fitted scale factor of 1.0069 0.0002. Comparisons of literature intensity values to our results reveal systematic deviations ranging from 1.16 % to +0.33 %.
34 pages, 10 figures, 4 tables, 54 references