Show simple item record

contributor authorColby, Frank P.
date accessioned2017-06-09T14:21:49Z
date available2017-06-09T14:21:49Z
date copyright1980/09/01
date issued1980
identifier issn0022-4928
identifier otherams-18002.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153960
description abstractPrevious investigations of the 8 June 1966 National Severe Storms Laboratory case show that mesoscale lift from an ?inland sea breeze? due to a newly formed temperature gradient preceded convection. Using additional surface data, this case was reanalyzed over all of Oklahoma. Cloud work functions were calculated from real and interpolated data to measure convective instability. The results indicated that the above temperature gradient was the eastern one of two gradients located on either side of a warm tongue. The cells formed over the eastern gradient where the convective instability was highest.
publisherAmerican Meteorological Society
titleThe Role of Convective Instability in an Oklahoma Squall Line
typeJournal Paper
journal volume37
journal issue9
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1980)037<2113:TROCII>2.0.CO;2
journal fristpage2113
journal lastpage2119
treeJournal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 009
contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record