Automated Retrievals of Water Vapor and Aerosol Profiles from an Operational Raman Lidar

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Tropospheric water vapor, convection, and climate (2010, background): “Lidars have been deployed only occasionally in field programs [Eichinger et al., 1999; Whiteman et al., 2006;Wulfmeyer et al., 2006], but they have shown robustness in long‐term monitoring sites [e.g., Turner et al., 2002; Ferrare et al., 2006].”
Multiyear aerosol observations with dual‐wavelength Raman lidar in the framework of EARLINET (2004, methodology): “Method B was suggested by Ferrare et al. [2001] and Turner et al. [2002] and can be regarded as the optimum one because the most appropriate lidar ratio is considered.”
Portable Raman Lidar Polly XT for Automated Profiling of Aerosol Backscatter, Extinction, and Depolarization (2009, methodology): “This is done similarly to Turner et al. (2002) by using the aerosol scattering ratio ASR(z) 5 [bMl(z) 1 b P l(z)]/b M l(z) ’ Pl0 (z)/PlR(z), where bl M(z) is the molecular backscatter coefficient.”
Enhancement of aerosol characterization using synergy of lidar and sun - photometer coincident observations: the GARRLiC algorithm (2013, background): “…observation can be achieved by employing lidar systems registering combined elastic-Raman signals (Ansmann et al., 1992; Ferrare et al., 1998a,b; Turner et al., 2002; Müller et al., 2007) or by conducting high spectral resolution idar observations (Shipley et al., 1983; Liu et al., 2002; Hair…”