Matching radiative transfer models and radiosonde data from the EPS/Metop Sodankylä campaign to IASI measurements
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 an...
| Published in: | Atmospheric Measurement Techniques |
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| Main Authors: | , , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Copernicus Publications
2011
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| Subjects: | |
| Online Access: | https://doi.org/10.5194/amt-4-1177-2011 https://noa.gwlb.de/receive/cop_mods_00027256 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00027211/amt-4-1177-2011.pdf https://amt.copernicus.org/articles/4/1177/2011/amt-4-1177-2011.pdf |
| Summary: | 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 ≤ ν ≤ 1570 and 1615 ≤ ν ≤ 1800 cm−1). |
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