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On Ice-Crystal Production by Aerosol Particles

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dc.contributor.authorFletcher, Neville H.
dc.date.accessioned2020-11-03T05:06:37Z
dc.date.issued1959
dc.description.abstractA general theory of the action of small aerosol particles as ice-crystal nuclei is developed and its predictions compared with experiment. It is found possible to decide under what conditions a given particle will act as a sublimation or as a freezing nucleus, and it is concluded that silver iodide generally behaves as a sublimation nucleus. The size effect is used to explain the activity distribution of silver iodide smoke, and this in turn explains the time lag observed in the nucleation of ice crystals by this smoke.en_AU
dc.format.mimetypeapplication/pdfen_AU
dc.identifier.issn0022-4928en_AU
dc.identifier.urihttp://hdl.handle.net/1885/213310
dc.language.isoen_AUen_AU
dc.publisherAmerican Meteorological Societyen_AU
dc.rights© 1959 American Meteorological Societyen_AU
dc.sourceThe Journal of the Atmospheric Sciencesen_AU
dc.titleOn Ice-Crystal Production by Aerosol Particlesen_AU
dc.typeJournal articleen_AU
dcterms.accessRightsOpen Accessen_AU
local.bibliographicCitation.issue2en_AU
local.bibliographicCitation.lastpage180en_AU
local.bibliographicCitation.startpage173en_AU
local.description.embargo2037-12-31
local.description.notesThe author was affiliated with University of New England when the paper was publisheden_AU
local.identifier.citationvolume16en_AU
local.identifier.doi10.1175/1520-0469(1959)016<0173:OICPBA>2.0.CO;2en_AU
local.publisher.urlhttp://www.ametsoc.org/pubs/journals/jas/index.htmlen_AU
local.type.statusPublished Versionen_AU

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