Cloud pressure retrieval using the O2‐O2 absorption band at 477 nm

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Science objectives of the ozone monitoring instrument (2006, background): “cloud information includes both the effective cloud coverage and effective cloud pressure, which employs absorption by O -O [22] and the rotational Raman scattering [23].”
Effective cloud fractions from the Ozone Monitoring Instrument: Theoretical framework and validation (2008, methodology): “In order to guide users, a summary of the validation status of effective cloud fraction and cloud pressure from the OMCLDO2 and OMCLDRR cloud products is presented.”
Retrieval of large volcanic SO2 columns from the Aura Ozone Monitoring Instrument: Comparison and limitations (2007, methodology): “Fortunately, cloud pressures consistent with the MLER model are being retrieved from OMI using approaches based on RRS [Joiner et al., 2004, 2006; Vasilkov et al., 2004] or absorption in the O2 O2 band near 477 nm [Acarreta et al., 2004].”
Updated Smithsonian Astrophysical Observatory Ozone Monitoring Instrument (SAO OMI) formaldehyde retrieval (2015, methodology): “Acarreta et al. (2004) estimated the systematic uncertainty of the cloud fraction to be ±0.1.”