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dc.contributor.authorPhillips, B. B.
dc.contributor.authorKinzer, Gilbert D.
dc.date.accessioned2017-06-09T14:11:56Z
dc.date.available2017-06-09T14:11:56Z
dc.date.copyright1958/08/01
dc.date.issued1958
dc.identifier.issn0095-9634
dc.identifier.otherams-14456.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150019
dc.description.abstractThe size and the free electric charge of more than 6000 individual natural cloud droplets have been measured. The measurements were made at a mountain laboratory in southeastern United States in strato-cumulus clouds and in thunderstorm-associated clouds. Stratocumulus clouds with fair-weather electric fields were found to have approximate Gaussian-charge distributions symmetric about zero charge. The magnitude and distribution of charge observed on these non-storm clouds approach values described recently by R. Gunn in his theory of aerosol electrification by the diffusion of environmental light ions. Thundercloud droplets were highly electrified and within given cloud volumes the droplets were charged entirely positive, entirely negative, or fractionally positive and negative.
dc.publisherAmerican Meteorological Society
dc.titleMEASUREMENTS OF THE SIZE AND ELECTRIFICATION OF DROPLETS IN CUMULIFORM CLOUDS
dc.typeJournal Paper
dc.journal.volume15
dc.journal.issue4
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1958)015<0369:MOTSAE>2.0.CO;2
dc.journal.fristpage369
dc.journal.lastpage374
dc.treeJournal of Meteorology:;1958:;volume( 015 ):;issue: 004
dc.contenttypeFulltext


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