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dc.contributor.authorCramer, Harrison E.
dc.contributor.authorRecord, Frank A.
dc.date.accessioned2017-06-09T14:11:12Z
dc.date.available2017-06-09T14:11:12Z
dc.date.copyright1955/04/01
dc.date.issued1955
dc.identifier.issn0095-9634
dc.identifier.otherams-14151.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149681
dc.description.abstractPower spectra of the eddy-velocity components have been determined at four levels within the layer from 2 to 12 meters under varying conditions of mean wind speed, trajectory and thermal stability. A filtering technique suggested by J. W. Tukey has been used to obtain rough estimates of contributions to the total variance for seven consecutive frequency intervals within the range from about 0.5 to 0.005 cycles per second. At the higher frequencies studied, variances for all three components are approximately equal and equipartition of turbulent energy is thus indicated. Spectra for the u- and v-components appear to be invariant with frequency at the lowest level, and tend to increase slowly with decreasing frequency at the higher levels. The w-spectra at all levels fall off sharply with decreasing frequency, contributions to the vertically-directed energy becoming almost negligible at the lowest frequencies investigated.
dc.publisherAmerican Meteorological Society
dc.titlePOWER SPECTRA OF THE EDDY-VELOCITY COMPONENTS
dc.typeJournal Paper
dc.journal.volume12
dc.journal.issue2
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1955)012<0146:PSOTEV>2.0.CO;2
dc.journal.fristpage146
dc.journal.lastpage151
dc.treeJournal of Meteorology:;1955:;volume( 012 ):;issue: 002
dc.contenttypeFulltext


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