The water vapor self-continuum absorption at 8.45 µm by optical feedback cavity ring down spectroscopy

• Published in: Journal of quantitative spectroscopy & radiative transfer Vol. 315; p. 108875
• Main Authors: Fournier, Q., Kassi, S., Mondelain, D., Fleurbaey, H., Georges, R., Campargue, A.
• Format: Journal Article
• Language: English
• Published: Elsevier 01-03-2024
• Subjects: Chemical Physics; Physics; CRDS; optical feedback; transparency window; Water vapor; continuum absorption; MT_CKD model
• ISSN: 0022-4073
• DOI: 10.1016/j.jqsrt.2023.108875

The accurate knowledge of the water vapor absorption in the 10 µm atmospheric window is of strong importance because this spectral range coincides with the maximum black body emission of Earth. Presently, the water vapor self-continuum is measured at the 1185 cm−1 (8.45 µm) spectral point, located in the most transparent interval of the 10 µm window. Measurements are performed at four temperatures ranging from 296 to 308 K using a newly developed Optical Feedback Cavity Ring Down Spectrometer (OF-CRDS). Self-continuum cross-sections, CS, are derived from the pressure dependence of the absorption during pressure ramps of pure water vapor up to 18 mbar. From the quadratic pressure dependence observed for the absorption coefficient at each temperature, we derived the value of the cross-section (Cs=0.996(12) × 10−22 cm2molecule−1atm−1 at 296 K) and its temperature dependence. These results are discussed in relation with previous literature measurements available in the 10 µm window. Our cross-section is found about 20% smaller than the MT_CKD_4.1 value and the available experimental works seem to indicate that the MT_CKD_4.1 temperature dependence is overestimated.