DIFFERENTIAL ADVECTION AS A FACTOR IN CLEAR-AIR TURBULENCE

dc.contributor.author	Keitz, Edwin L.
dc.date.accessioned	2017-06-09T14:12:03Z
dc.date.available	2017-06-09T14:12:03Z
dc.date.copyright	1959/02/01
dc.date.issued	1959
dc.identifier.issn	0095-9634
dc.identifier.other	ams-14493.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4150060
dc.description.abstract	Clear-air turbulence observations made by accelerometer measurements have been correlated with six-hour forecasts of the change in vertical stability. The change in stability has been forecast by computing the six-hour horizontal temperature advection at two levels. By means of the Kolmogorov-Smirnov non-parametric test for cumulative distributions, a significant correlation has been shown to exist between the observations of turbulence and the forecast change in stability. However, no significance has been established regarding the magnitude of the turbulence.
dc.publisher	American Meteorological Society
dc.title	DIFFERENTIAL ADVECTION AS A FACTOR IN CLEAR-AIR TURBULENCE
dc.type	Journal Paper
dc.journal.volume	16
dc.journal.issue	1
dc.journal.title	Journal of Meteorology
dc.identifier.doi	10.1175/1520-0469(1959)016<0057:DAAAFI>2.0.CO;2
dc.journal.fristpage	57
dc.journal.lastpage	62
dc.tree	Journal of Meteorology:;1959:;volume( 016 ):;issue: 001
dc.contenttype	Fulltext