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dc.contributor.authorMunn, R. E.
dc.date.accessioned2017-06-09T14:12:30Z
dc.date.available2017-06-09T14:12:30Z
dc.date.copyright1961/02/01
dc.date.issued1961
dc.identifier.issn0095-9634
dc.identifier.otherams-14691.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150280
dc.description.abstractA theoretical expression is derived for the root-mean-square vertical-eddy fluctuation in terms of the friction velocity, the height and Monin and Obukhov's function ?. Steady-state conditions and constant shearing stress are assumed. It is shown that increases with height under superadiabatic conditions, is constant with height when the lapse rate is adiabatic and decreases with height during inversions. Indirect evidence suggests that the height variation of can be approximated by a power law.
dc.publisherAmerican Meteorological Society
dc.titleA THEORETICAL EXPRESSION FOR THE ROOT MEAN SQUARE VERTICAL EDDY FLUCTUATION
dc.typeJournal Paper
dc.journal.volume18
dc.journal.issue1
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1961)018<0038:ATEFTR>2.0.CO;2
dc.journal.fristpage38
dc.journal.lastpage42
dc.treeJournal of Meteorology:;1961:;volume( 018 ):;issue: 001
dc.contenttypeFulltext


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