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latest version, AERIoe, version 2.2, surface layer observations and observations from additional sources of upper-air thermodynamic profiles (e.g., radiosondes, NWP forecast soundings, Raman lidar) can be included within Y . The inclusion of NWP forecast soundings in the mid- to upper troposphere improves the overall retrieval as short-term forecast models are often most accurate at these altitudes ( Thompson et al. 2003 ; Benjamin et al. 2004a , b ). The intent of including these observations in
latest version, AERIoe, version 2.2, surface layer observations and observations from additional sources of upper-air thermodynamic profiles (e.g., radiosondes, NWP forecast soundings, Raman lidar) can be included within Y . The inclusion of NWP forecast soundings in the mid- to upper troposphere improves the overall retrieval as short-term forecast models are often most accurate at these altitudes ( Thompson et al. 2003 ; Benjamin et al. 2004a , b ). The intent of including these observations in
