SN
Slobodan Nichovic
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1
Conference paper
(2018)
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Eleni Marinou, Vassilis Amiridis, Holger Baars, Michael Kottas, Alexandra Tsekeri, Emmanouil Proestakis, Panagiotis Kokkalis, Philippe Goloub, Bojan Cvetkovic, Slobodan Nichovic, Rodanthi Mamouri, Michael Pikridas, Albert Ansmann, Iasonas Stavroulas, Christos Keleshis, Jean Sciare, Athanasios Nenes, Dimitris Balis, Jann Schrod, Ioannis Binietoglou, Stavros Solomos, Dimitra Mamali, Ronny Engelmann
By means of available ice nucleating particle (INP) parameterization schemes we compute profiles of dust INP number concentration utilizing Polly-XT and CALIPSO lidar observations during the INUIT-BACCHUS-ACTRIS 2016 campaign. The polarization-lidar photometer networking (POLIPHON) method is used to separate dust and non-dust aerosol backscatter, extinction, mass concentration, particle number concentration (for particles with radius > 250 nm) and surface area concentration. The INP final products are compared with aerosol samples collected from unmanned aircraft systems (UAS) and analyzed using the ice nucleus counter FRIDGE.
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By means of available ice nucleating particle (INP) parameterization schemes we compute profiles of dust INP number concentration utilizing Polly-XT and CALIPSO lidar observations during the INUIT-BACCHUS-ACTRIS 2016 campaign. The polarization-lidar photometer networking (POLIPHON) method is used to separate dust and non-dust aerosol backscatter, extinction, mass concentration, particle number concentration (for particles with radius > 250 nm) and surface area concentration. The INP final products are compared with aerosol samples collected from unmanned aircraft systems (UAS) and analyzed using the ice nucleus counter FRIDGE.