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contributor authorDJURIC, DUŠAN
date accessioned2017-06-09T15:59:11Z
date available2017-06-09T15:59:11Z
date copyright1969/12/01
date issued1969
identifier issn0027-0644
identifier otherams-58152.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198568
description abstractAn interpretation of the ?-equation shows that upward motion is closely related to the advection of vorticity in the upper troposphere and to warm advection in the lower troposphere. Examples are presented to illustrate both effects.
publisherAmerican Meteorological Society
titleNOTE ON ESTIMATION OF VERTICAL MOTION BY THE OMEGA EQUATION
typeJournal Paper
journal volume97
journal issue12
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1969)097<0902:NOEOVM>2.3.CO;2
journal fristpage902
journal lastpage904
treeMonthly Weather Review:;1969:;volume( 097 ):;issue: 012
contenttypeFulltext


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