Heterogeneous nucleation of ice particles on glassy aerosols under cirrus conditions
Ice clouds in the tropical tropopause layer have a key role in dehydrating air that is entering the stratosphere. Cloud-chamber measurements suggest that their high humidity can be explained if heterogeneous ice nucleation on glassy aerosols is a significant nucleation mechanism in this region.
Gespeichert in:
| Hauptverfasser: | , , , , , , , , , , , , , |
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| Dokumenttyp: | Article (Journal) |
| Sprache: | Englisch |
| Veröffentlicht: |
21 March 2010
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| In: |
Nature geoscience
Year: 2010, Jahrgang: 3, Heft: 4, Pages: 233-237 |
| ISSN: | 1752-0908 |
| DOI: | 10.1038/ngeo817 |
| Online-Zugang: | Verlag, lizenzpflichtig, Volltext: https://doi.org/10.1038/ngeo817 Verlag, lizenzpflichtig, Volltext: https://www.nature.com/articles/ngeo817 
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| Verfasserangaben: | Benjamin J. Murray, Theodore W. Wilson, Steven Dobbie, Zhiqiang Cui, Sardar M. R. K. Al-Jumur, Ottmar Möhler, Martin Schnaiter, Robert Wagner, Stefan Benz, Monika Niemand, Harald Saathoff, Volker Ebert, Steven Wagner, and Bernd Kärcher |
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| 520 | |a Ice clouds in the tropical tropopause layer have a key role in dehydrating air that is entering the stratosphere. Cloud-chamber measurements suggest that their high humidity can be explained if heterogeneous ice nucleation on glassy aerosols is a significant nucleation mechanism in this region. | ||
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