THE ELECTRIC CHARGE ON CONDENSATE AND WATER DROPLETS

dc.contributor.author	Magono, Choji
dc.contributor.author	Takahashi, Tsutomu
dc.date.accessioned	2017-06-09T14:12:05Z
dc.date.available	2017-06-09T14:12:05Z
dc.date.copyright	1959/04/01
dc.date.issued	1959
dc.identifier.issn	0095-9634
dc.identifier.other	ams-14507.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4150076
dc.description.abstract	It was found that dew produced artificially on a thin wire was electrified negatively when the water temperature of the reservoir for supplying water vapor was lower than about 80C and positively when the temperature was higher than about 85C. The electrification phenomena of the condensate were considered to be originated from the electric charge on individual water droplets, because it was observed that the droplets were electrified when they rose from the water surface of the reservoir, and the sign of charge on the individual droplets agreed well with that of the condensate.
dc.publisher	American Meteorological Society
dc.title	THE ELECTRIC CHARGE ON CONDENSATE AND WATER DROPLETS
dc.type	Journal Paper
dc.journal.volume	16
dc.journal.issue	2
dc.journal.title	Journal of Meteorology
dc.identifier.doi	10.1175/1520-0469(1959)016<0167:TECOCA>2.0.CO;2
dc.journal.fristpage	167
dc.journal.lastpage	173
dc.tree	Journal of Meteorology:;1959:;volume( 016 ):;issue: 002
dc.contenttype	Fulltext