“…The usefulness of measuring atmospheric T and WV in order to diagnose the state of the atmosphere lead to the development of satellite‐based sounding instruments over 40 years ago [ Hilleary et al , 1966; James , 1967; Yates , 1970; Chesters et al , 1986], beginning with the U.S. Satellite Infrared Spectrometer (SIRS) and Infrared Interferometer Spectrometer (IRIS) onboard Nimbus 3, launched in 1969 [ Wark and Hilleary , 1969; Hayden , 1971; Wick , 1971; Smith , 1972]. SIRS and IRIS were capable of remotely sensing atmospheric T structures by using statistical relationships and regression methods [ Kaplan et al , 1977; Westwater and Strand , 1968; Smith et al , 1970; Crosby et al , 1973; Fritz , 1977].…”