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Characterization of aerosol particles at Cabo Verde close to sea level and at the cloud level – Part 2: Ice-nucleating particles in air, cloud and seawater

Ice-nucleating particles (INPs) in the troposphere can form ice in clouds via heterogeneous ice nucleation. Yet, atmospheric number concentrations of INPs (N.sub.INP) are not well characterized, and, although there is some understanding of their sources, it is still unclear to what extend different...

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Published in:Atmospheric chemistry and physics 2020-02, Vol.20 (3), p.1451-1468
Main Authors: Gong, Xianda, Wex, Heike, van Pinxteren, Manuela, Triesch, Nadja, Fomba, Khanneh Wadinga, Lubitz, Jasmin, Stolle, Christian, Robinson, Tiera-Brandy, Müller, Thomas, Herrmann, Hartmut, Stratmann, Frank
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Language:English
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Summary:Ice-nucleating particles (INPs) in the troposphere can form ice in clouds via heterogeneous ice nucleation. Yet, atmospheric number concentrations of INPs (N.sub.INP) are not well characterized, and, although there is some understanding of their sources, it is still unclear to what extend different sources contribute or if all sources are known. In this work, we examined properties of INPs at Cabo Verde (a.k.a. Cape Verde) from different environmental compartments: the oceanic sea surface microlayer (SML), underlying water (ULW), cloud water and the atmosphere close to both sea level and cloud level.
ISSN:1680-7324
1680-7316
1680-7324
DOI:10.5194/acp-20-1451-2020