A Preliminary Study of Ice Grown by Droplet Accretion Using Water-Insoluble Particles as Tracer

dc.contributor.author	Prodi, F.
dc.contributor.author	Nagamoto, C. T.
dc.contributor.author	Rosinski, J.
dc.date.accessioned	2017-06-09T17:40:23Z
dc.date.available	2017-06-09T17:40:23Z
dc.date.copyright	1980/03/01
dc.date.issued	1979
dc.identifier.issn	0021-8952
dc.identifier.other	ams-9869.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4233404
dc.description.abstract	The migration of water-insoluble particles during freezing was used to study the structure of ice grown by droplet accretion. Experiments were performed in a cold tunnel under different growth conditions using nickel powder as a tracer; the resulting deposit was examined using the x-ray microradiograph technique. Analysis of the types of tracer particle aggregates provided a description of the freezing processes. It was concluded that this method could be used as an additional tool in studies of the various ice growth conditions found in nature.
dc.publisher	American Meteorological Society
dc.title	A Preliminary Study of Ice Grown by Droplet Accretion Using Water-Insoluble Particles as Tracer
dc.type	Journal Paper
dc.journal.volume	19
dc.journal.issue	3
dc.journal.title	Journal of Applied Meteorology
dc.identifier.doi	10.1175/1520-0450(1980)019<0284:APSOIG>2.0.CO;2
dc.journal.fristpage	284
dc.journal.lastpage	289
dc.tree	Journal of Applied Meteorology:;1979:;volume( 019 ):;issue: 003
dc.contenttype	Fulltext