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dc.contributor.authorEdinger, J. G.
dc.contributor.authorRapp, R. R.
dc.date.accessioned2017-06-09T14:11:43Z
dc.date.available2017-06-09T14:11:43Z
dc.date.copyright1957/10/01
dc.date.issued1957
dc.identifier.issn0095-9634
dc.identifier.otherams-14371.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149925
dc.description.abstractTransosonde balloon data are analyzed to provide a measure of the dispersion on a large scale in the upper atmosphere. An expression for the autocorrelation function is inferred from synoptic experience and is applied to autocorrelation values computed from the balloon data. Taylor's theorem is applied to this function to compute dispersion out to ten days. A comparison is made with direct computation at two days.
dc.publisherAmerican Meteorological Society
dc.titleDISPERSION IN THE UPPER ATMOSPHERE
dc.typeJournal Paper
dc.journal.volume14
dc.journal.issue5
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1957)014<0421:DITUA>2.0.CO;2
dc.journal.fristpage421
dc.journal.lastpage425
dc.treeJournal of Meteorology:;1957:;volume( 014 ):;issue: 005
dc.contenttypeFulltext


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