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contributor authorShackford, Charles Reeve
date accessioned2017-06-09T14:12:16Z
date available2017-06-09T14:12:16Z
date copyright1960/02/01
date issued1960
identifier issn0095-9634
identifier otherams-14590.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150168
description abstractThunderstorm electrical activity in terms of surface-observed lightning-stroke rate is related to that radar-reflectivity maxima above the 0C level and to vertical profiles of radar reflectivity. This, and the fact it is also related to the incidence of hail at the surface, lends support to a previously stated theory of charge generation and separation by Workman and Reynolds. Observer data show an order of events at the surface which indicates a thunderstorm structure coinciding with previous models.
publisherAmerican Meteorological Society
titleRADAR INDICATIONS OF A PRECIPITATION-LIGHTNING RELATIONSHIP IN NEW ENGLAND THUNDERSTORMS
typeJournal Paper
journal volume17
journal issue1
journal titleJournal of Meteorology
identifier doi10.1175/1520-0469(1960)017<0015:RIOAPL>2.0.CO;2
journal fristpage15
journal lastpage19
treeJournal of Meteorology:;1960:;volume( 017 ):;issue: 001
contenttypeFulltext


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