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

Conference Paper (2018)
Author(s)

Eleni Marinou (Aristotle University of Thessaloniki, National Observatory of Athens)

Vassilis Amiridis (National Observatory of Athens)

Albert Ansmann (Leibniz-Institut für Troposphärenforschung)

Athanasios Nenes (National Observatory of Athens, FORTH, Georgia Institute of Technology)

Dimitris Balis (Aristotle University of Thessaloniki)

Jann Schrod (Goethe University)

Ioannis Binietoglou (National Observatory of Athens, National Institute of RandD for Optoelectronics)

Stavros Solomos (National Observatory of Athens)

Dimitra Mamali (TU Delft - Atmospheric Remote Sensing)

Ronny Engelmann (Leibniz-Institut für Troposphärenforschung)

Holger Baars (Leibniz-Institut für Troposphärenforschung)

Michael Kottas (National Observatory of Athens)

Alexandra Tsekeri (National Observatory of Athens)

Emmanouil Proestakis (National Observatory of Athens, University of Patras)

Panagiotis Kokkalis (National Observatory of Athens)

Philippe Goloub (Universite Lille-1)

Bojan Cvetkovic (Republic Hydrometeorological Service of Serbia)

Slobodan Nichovic (Republic Hydrometeorological Service of Serbia)

Rodanthi Mamouri (Cyprus University of Technology, Energy)

Michael Pikridas (Energy)

Iasonas Stavroulas (Energy)

Christos Keleshis (Energy)

Jean Sciare (Energy)

Research Group
Atmospheric Remote Sensing
DOI related publication
https://doi.org/10.1051/epjconf/201817605018 Final published version
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Publication Year
2018
Language
English
Research Group
Atmospheric Remote Sensing
Volume number
176
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358
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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.