Heterogeneous ice nucleation of viscous secondary organic aerosol produced from ozonolysis of α-pinene

There are strong indications that particles containing secondary organic aerosol (SOA) exhibit amorphous solid or semi-solid phase states in the atmosphere. This may facilitate heterogeneous ice nucleation and thus influence cloud properties. However, experimental ice nucleation studies of biogenic...

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Bibliographic Details
Main Authors: Ignatius, Karoliina (Author), Kristensen, Thomas B. (Author), Järvinen, Emma (Author), Nichman, Leonid (Author), Fuchs, Claudia (Author), Gordon, Hamish (Author), Herenz, Paul (Author), Hoyle, Christopher R. (Author), Duplissy, Jonathan (Author), Garimella, Sarvesh (Contributor), Dias, Antonio (Author), Frege, Carla (Author), Höppel, Niko (Author), Tröstl, Jasmin (Author), Wagner, Robert (Author), Yan, Chao (Author), Amorim, Antonio (Author), Baltensperger, Urs (Author), Curtius, Joachim (Author), Donahue, Neil M. (Author), Gallagher, Martin W. (Author), Kirkby, Jasper (Author), Kulmala, Markku (Author), Möhler, Ottmar (Author), Saathoff, Harald (Author), Schnaiter, Martin (Author), Tomé, Antonio (Author), Virtanen, Annele (Author), Worsnop, Douglas (Author), Stratmann, Frank (Author)
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor)
Format: Article
Language:English
Published: Copernicus GmbH, 2016-12-29T20:33:27Z.
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