Lidar Ice nuclei estimates and how they relate with airborne in-situ measurements

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...

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Published inEPJ Web of Conferences Vol. 176; p. 5018
Main Authors Marinou, Eleni, Amiridis, Vassilis, Ansmann, Albert, Nenes, Athanasios, Balis, Dimitris, Schrod, Jann, Binietoglou, Ioannis, Solomos, Stavros, Mamali, Dimitra, Engelmann, Ronny, Baars, Holger, Kottas, Michael, Tsekeri, Alexandra, Proestakis, Emmanouil, Kokkalis, Panagiotis, Goloub, Philippe, Cvetkovic, Bojan, Nichovic, Slobodan, Mamouri, Rodanthi, Pikridas, Michael, Stavroulas, Iasonas, Keleshis, Christos, Sciare, Jean
Format Journal Article Conference Proceeding
LanguageEnglish
Published Les Ulis EDP Sciences 01.01.2018
Subjects
Airborne particulates
Airborne sensing
Backscattering
Dust
Ice nuclei
Lidar
Parameterization
Unmanned aircraft
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Abstract 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.
AbstractList 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.
Author Mamali, Dimitra
Nenes, Athanasios
Mamouri, Rodanthi
Pikridas, Michael
Marinou, Eleni
Binietoglou, Ioannis
Kokkalis, Panagiotis
Proestakis, Emmanouil
Balis, Dimitris
Cvetkovic, Bojan
Kottas, Michael
Stavroulas, Iasonas
Engelmann, Ronny
Ansmann, Albert
Nichovic, Slobodan
Goloub, Philippe
Sciare, Jean
Tsekeri, Alexandra
Schrod, Jann
Keleshis, Christos
Solomos, Stavros
Amiridis, Vassilis
Baars, Holger
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10.5194/acp-2016-1098
10.1007/978-94-017-8978-3
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R3
Mamouri (R5) 2016; 16
Nickovic (R4) 2001; 106
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Engelmann (R2) 2016; 9
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Snippet By means of available ice nucleating particle (INP) parameterization schemes we compute profiles of dust INP number concentration utilizing Polly-XT and...
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SubjectTerms Airborne particulates
Airborne sensing
Backscattering
Dust
Ice nuclei
Lidar
Parameterization
Unmanned aircraft
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Title Lidar Ice nuclei estimates and how they relate with airborne in-situ measurements
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