On the role of ice-nucleating aerosol in the formation of ice particles in tropical mesoscale convective systems

Over decades, the cloud physics community has debated the nature and role of aerosol particles in ice initiation. The present study shows that the measured concentration of ice crystals in tropical mesoscale convective systems exceeds the concentration of ice nucleating particles (INPs) by several o...

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Détails bibliographiques
Publié dans:Geophysical research letters. - 1984. - 44(2017), 3 vom: 16. Feb., Seite 1574-1582
Auteur principal: Ladino, Luis A (Auteur)
Autres auteurs: Korolev, Alexei, Heckman, Ivan, Wolde, Mengistu, Fridlind, Ann M, Ackerman, Andrew S
Format: Article en ligne
Langue:English
Publié: 2017
Accès à la collection:Geophysical research letters
Sujets:Journal Article ice nucleating particles mesoscale convective systems secondary ice production
Description
Résumé:Over decades, the cloud physics community has debated the nature and role of aerosol particles in ice initiation. The present study shows that the measured concentration of ice crystals in tropical mesoscale convective systems exceeds the concentration of ice nucleating particles (INPs) by several orders of magnitude. The concentration of INPs was assessed from the measured aerosol particles concentration in the size range of 0.5 to 1 µm. The observations from this study suggest that primary ice crystals formed on INPs make only a minor contribution to the total concentration of ice crystals in tropical mesoscale convective systems. This is found by comparing the predicted INP number concentrations with in-situ ice particle number concentrations. The obtained measurements suggest that ice multiplication is the likely explanation for the observed high concentrations of ice crystals in this type of convective system
Description:Date Revised 20.11.2019
published: Print-Electronic
Citation Status PubMed-not-MEDLINE
ISSN:0094-8276
DOI:10.1002/2016GL072455