THE VERTICAL DISTRIBUTION OF SUB-MICRON PARTICLES IN THE STRATOSPHERE

dc.contributor.author	Chagnon, Charles W.
dc.contributor.author	Junge, Christian E.
dc.date.accessioned	2017-06-09T14:12:45Z
dc.date.available	2017-06-09T14:12:45Z
dc.date.copyright	1961/12/01
dc.date.issued	1961
dc.identifier.issn	0095-9634
dc.identifier.other	ams-14788.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4150387
dc.description.abstract	The vertical distribution of stratospheric particles with an average radius of 0.15 micron is presented in the form of five vertical profiles. These show a broad maximum in numerical concentration between 15 and 23 km, and are remarkably consistent throughout the one-year period of observations from November, 1959 to October, 1960. It is suggested that this ?aerosol layer? is identical to the particles responsible for the ?purple light? phenomenon, and the haze layers observed in the stratosphere. Some pertinent details of the balloon-borne collection instruments are included.
dc.publisher	American Meteorological Society
dc.title	THE VERTICAL DISTRIBUTION OF SUB-MICRON PARTICLES IN THE STRATOSPHERE
dc.type	Journal Paper
dc.journal.volume	18
dc.journal.issue	6
dc.journal.title	Journal of Meteorology
dc.identifier.doi	10.1175/1520-0469(1961)018<0746:TVDOSM>2.0.CO;2
dc.journal.fristpage	746
dc.journal.lastpage	752
dc.tree	Journal of Meteorology:;1961:;volume( 018 ):;issue: 006
dc.contenttype	Fulltext