Secondary Ice Formation in Idealised Deep Convection—Source of Primary Ice and Impact on Glaciation
Secondary ice production via rime-splintering is considered to be an important process for rapid glaciation and high ice crystal numbers observed in mixed-phase convective clouds. An open question is how rime-splintering is triggered in the relatively short time between cloud formation and observati...
Main Authors: | Annette K. Miltenberger, Tim Lüttmer, Christoph Siewert |
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Format: | Article |
Language: | English |
Published: |
MDPI AG
2020-05-01
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Series: | Atmosphere |
Subjects: | |
Online Access: | https://www.mdpi.com/2073-4433/11/5/542 |
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