Homogeneous ice formation in convective cloud outflow regions
Homogeneous droplet freezing in the warm cirrus regime (230–240 K) is investigated along idealized convective cloud trajectories using a spectral parcel model developed to track droplet freezing events accurately. The novel model is described and used to study ice formation from rapidly ascending (v...
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Veröffentlicht in: | Quarterly journal of the Royal Meteorological Society 2017-07, Vol.143 (706), p.2093-2103 |
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Format: | Artikel |
Sprache: | eng |
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