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Radiances observed from IASI are compared to calculated ones.  Calculated radiances are obtained using several radiative  transfer models (OSS, LBLRTM v11.3 and v11.6) on best  estimates of the atmospheric state vectors. The atmospheric  state vectors are derived from cryogenic frost point  hygrometer and humidity dry bias corrected RS92 measurements  flown on sondes launched 1 h and 5 min before IASI  overpass time. The temperature and humidity best estimate  profiles are  obtained by interpolating or extrapolating these  measurements to IASI overpass time. The IASI observed and  calculated radiances match to within one sigma IASI instrument  noise in the spectral region where water vapour is a strong  absorber (wavenumber, ν, in the range of 1500 &le; &nu; &le;  1570 and 1615 &le; &nu; &le; 1800 cm<sup>−1</sup>)

Matching radiative transfer models and radiosonde data from the EPS/Metop Sodankylä campaign to IASI measurements