ATMOSPHERIC DIFFUSION FROM VOLUME SOURCES

dc.contributor.author	Gifford, Frank
dc.date.accessioned	2017-06-09T14:11:14Z
dc.date.available	2017-06-09T14:11:14Z
dc.date.copyright	1955/06/01
dc.date.issued	1955
dc.identifier.issn	0095-9634
dc.identifier.other	ams-14167.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4149698
dc.description.abstract	Under the assumption of homogeneous and isotropic turbulence, an equation is obtained for diffusion from an instantaneous volume source that has spherical symmetry but otherwise a virtually arbitrary initial distribution. Several special cases are fully developed and compared, the most general being one in which the initial maximum concentration may occur away from the center of the source.
dc.publisher	American Meteorological Society
dc.title	ATMOSPHERIC DIFFUSION FROM VOLUME SOURCES
dc.type	Journal Paper
dc.journal.volume	12
dc.journal.issue	3
dc.journal.title	Journal of Meteorology
dc.identifier.doi	10.1175/1520-0469(1955)012<0245:ADFVS>2.0.CO;2
dc.journal.fristpage	245
dc.journal.lastpage	251
dc.tree	Journal of Meteorology:;1955:;volume( 012 ):;issue: 003
dc.contenttype	Fulltext