Spaceborne Evidence That Ice-Nucleating Particles Influence High-Latitude Cloud Phase

© 2022 The Authors.

Détails bibliographiques
Publié dans:Geophysical research letters. - 1984. - 49(2022), 14 vom: 28. Juli, Seite e2022GL098041
Auteur principal: Carlsen, Tim (Auteur)
Autres auteurs: David, Robert O
Format: Article en ligne
Langue:English
Publié: 2022
Accès à la collection:Geophysical research letters
Sujets:Journal Article Arctic Southern Ocean cloud phase ice‐nucleating particles mixed‐phase clouds satellite
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520 |a Mixed-phase clouds (MPCs), which consist of both supercooled cloud droplets and ice crystals, play an important role in the Earth's radiative energy budget and hydrological cycle. In particular, the fraction of ice crystals in MPCs determines their radiative effects, precipitation formation and lifetime. In order for ice crystals to form in MPCs, ice-nucleating particles (INPs) are required. However, a large-scale relationship between INPs and ice initiation in clouds has yet to be observed. By analyzing satellite observations of the typical transition temperature (T*) where MPCs become more frequent than liquid clouds, we constrain the importance of INPs in MPC formation. We find that over the Arctic and Southern Ocean, snow and sea ice cover significantly reduces T*. This indicates that the availability of INPs is essential in controlling cloud phase evolution and that local sources of INPs in the high-latitudes play a key role in the formation of MPCs 
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