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
1. Verfasser: Karcher, B
Format: Artikel
Sprache:eng
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