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contributor authorPaluch, Ilga R.
contributor authorSartor, J. Doyne
date accessioned2017-06-09T14:17:07Z
date available2017-06-09T14:17:07Z
date copyright1973/09/01
date issued1973
identifier issn0022-4928
identifier otherams-16427.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152209
description abstractExpressions are derived for ice particle charges acquired through successive collisions in a changing electric field. Our computations give lower particle charges, slower maximum field growth rates, and higher maxium fields than reported in recent literature. The minimum ice particle sizes and concentrations required for efficient electrification appear to lie well within the range observed in thunderstorms. If the mean radius of the large ice particles (graupel, hail, etc.) exceeds 0.2 cm, fields higher than 5000 V cm?1 can be generated.
publisherAmerican Meteorological Society
titleThunderstorm Electrification by the Inductive Charging Mechanism:I. Particle Charges and Electric Fields
typeJournal Paper
journal volume30
journal issue6
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1973)030<1166:TEBTIC>2.0.CO;2
journal fristpage1166
journal lastpage1173
treeJournal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 006
contenttypeFulltext


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