RADAR INDICATIONS OF A PRECIPITATION-LIGHTNING RELATIONSHIP IN NEW ENGLAND THUNDERSTORMS

dc.contributor.author	Shackford, Charles Reeve
dc.date.accessioned	2017-06-09T14:12:16Z
dc.date.available	2017-06-09T14:12:16Z
dc.date.copyright	1960/02/01
dc.date.issued	1960
dc.identifier.issn	0095-9634
dc.identifier.other	ams-14590.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4150168
dc.description.abstract	Thunderstorm 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.
dc.publisher	American Meteorological Society
dc.title	RADAR INDICATIONS OF A PRECIPITATION-LIGHTNING RELATIONSHIP IN NEW ENGLAND THUNDERSTORMS
dc.type	Journal Paper
dc.journal.volume	17
dc.journal.issue	1
dc.journal.title	Journal of Meteorology
dc.identifier.doi	10.1175/1520-0469(1960)017<0015:RIOAPL>2.0.CO;2
dc.journal.fristpage	15
dc.journal.lastpage	19
dc.tree	Journal of Meteorology:;1960:;volume( 017 ):;issue: 001
dc.contenttype	Fulltext