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contributor authorZiv, Ami
contributor authorLevin, Zev
date accessioned2017-06-09T14:17:41Z
date available2017-06-09T14:17:41Z
date copyright1974/09/01
date issued1974
identifier issn0022-4928
identifier otherams-16636.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152441
description abstractA time-dependent numerical model is used to simulate the growth of the electric field in thunderclouds by the polarization mechanism, including both the growth of hydrometeors and the growth of the electric charge centers. The results demonstrate a direct coupling between the hydrometeor growth and the electric field. Different types of cloud are discussed with reference to their electrical behavior. It is found that clouds containing large ice particles and small supercooled water drops and fully glaciated clouds can produce electric fields sufficient for lightning to occur. Electrical forces in the clouds tend to slow down the relative fall velocities of the precipitation particles, and reduce their interaction rate. The net effect is a slowing down of the growth of the hydrometeors and the rate of buildup of the electric field.
publisherAmerican Meteorological Society
titleThundercloud Electrification: Cloud Growth and Electrical Development
typeJournal Paper
journal volume31
journal issue6
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1974)031<1652:TECGAE>2.0.CO;2
journal fristpage1652
journal lastpage1661
treeJournal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 006
contenttypeFulltext


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