Retrieval of stratospheric temperatures from Atmospheric Infrared Sounder radiance measurements for gravity wave studies

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A global view of stratospheric gravity wave hotspots located with Atmospheric Infrared Sounder observations (2012, methodology): “The number of channels at 15 mm, which are sensitive to temperature perturbations in the middle and upper stratosphere, is rather limited compared with the 4.3 mm band [Hoffmann and Alexander, 2009].”
Variability and predictability of the space environment as related to lower atmosphere forcing (2016, background): “…[Fetzer and Gille, 1994; Dewan et al., 1998; Tsuda et al., 2000; Eckermann and Preusse, 1999; Ern et al., 2004; Alexander et al., 2008; Wu and Eckermann, 2008; Hoffmann and Alexander, 2009; Ern et al., 2011; Gong et al., 2012; Sakanoi et al., 2011; Alexander, 2015; Miller et al., 2015].”