Multiyear aerosol observations with dual‐wavelength Raman lidar in the framework of EARLINET

By Ina Mattis, Albert Ansmann, Detlef Müller, Ulla Wandinger, Dietrich Althausen. 2004

185 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/06957f43442e984b9447a1754058ec635bef6118

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Citations in the corpus

Depolarization and lidar ratios at 355, 532, and 1064 nm and microphysical properties of aged tropospheric and stratospheric Canadian wildfire smoke (2018, methodology): “The second lidar was the dual receiver field-ofview (RFOV) multiwavelength polarization/Raman lidar MARTHA (Multiwavelength Tropospheric Raman lidar for Temperature, Humidity, and Aerosol profiling; Mattis et al., 2003, 2008; Schmidt et al., 2013, 2014; Jimenez et al., 2017).”
Portable Raman Lidar Polly XT for Automated Profiling of Aerosol Backscatter, Extinction, and Depolarization (2009, background): “…are based on our long-term experience in aerosol Raman lidar observations of clouds and aerosols (Ansmann et al. 1990, 1992; Althausen et al. 2000; Mattis et al. 2004, 2008; Müller et al. 2005) and on the numerous field campaigns we conducted during the past 10 yr in Europe (e.g., Ansmann et al.…”
Potential of polarization lidar to provide profiles of CCN- and INP-relevant aerosol parameters (2015, background): “On average, the free-tropospheric AOT contributes 20% to the overall AOT (Mattis et al., 2004).”
EARLINET correlative measurements for CALIPSO: First intercomparison results (2010, background): “…type, mixing state, and properties in the free troposphere and the local planetary boundary layer [e.g., Ansmann et al. 2003; Matthias et al. , 2004; Mattis et al. , 2004, 2008; Pappalardo et al. , 2004a; Mona et al. , 2006; Balis et al. , 2003; Wandinger et al. , 2004; Amiridis et al. , 2005;…”
Review of (2006, unknown): “These aerosol conditions match well with findings of Mattis et al. (2004) who presented aerosol lidar results for the boundary layer and lower free troposphere over the EARLINET station at Leipzig between 2000 and 2003.”
Ceilometer lidar comparison: backscatter coefficient retrieval and signal-to-noise ratio determination (2010, methodology): “For simplification, in this study a constant lidar ratio of 55 sr is assumed for both the lidar and the ceilometer that is valid for continental urban aerosol (Mattis et al. , 2004), for Saharan dust (Müller et al. , 2007), and for volcanic ash plumes over Europe (Ansmann et al. , 2010).”
Aerosol Properties and Processes: A Path from Field and Laboratory Measurements to Global Climate Models (2007, methodology): “…retrievals by the ARM Raman lidar (Ferrare et a l. 2006), AERONET (Holben et a l. 1998), MPLNET (Welton et al. 2002), and EARLINET (Bösenberg et al. 2003; Mattis et al. 2004) provide limited horizontal sampling, they also provide accuracy and vertical resolution lacking in satellite retrievals.”