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dc.contributor.authorGifford, Frank
dc.date.accessioned2017-06-09T14:11:28Z
dc.date.available2017-06-09T14:11:28Z
dc.date.copyright1956/06/01
dc.date.issued1956
dc.identifier.issn0095-9634
dc.identifier.otherams-14265.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149807
dc.description.abstractPreviously, analysis of the Eulerian time correlation has been restricted to the limiting cases of very small turbulence level (G. I. Taylor's hypothesis) and very large turbulence level. In the atmosphere, the turbulence level is generally intermediate. The time correlation is obtained for the case of arbitrary turbulence level, and several applications to both small- and large-scale atmospheric turbulent fluctuations are considered.
dc.publisherAmerican Meteorological Society
dc.titleTHE RELATION BETWEEN SPACE AND TIME CORRELATIONS IN THE ATMOSPHERE
dc.typeJournal Paper
dc.journal.volume13
dc.journal.issue3
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1956)013<0289:TRBSAT>2.0.CO;2
dc.journal.fristpage289
dc.journal.lastpage294
dc.treeJournal of Meteorology:;1956:;volume( 013 ):;issue: 003
dc.contenttypeFulltext


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