Show simple item record

dc.contributor.authorSaltsman, Barry
dc.date.accessioned2017-06-09T14:11:44Z
dc.date.available2017-06-09T14:11:44Z
dc.date.copyright1957/12/01
dc.date.issued1957
dc.identifier.issn0095-9634
dc.identifier.otherams-14385.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149940
dc.description.abstractBy considering the Fourier analysis of the planetary field of motion in the atmosphere, it is possible to define ?scales? of motion and to write equations which govern the behavior of these separate scales of motion. Specifically, equations for the rate of change of the kinetic and available potential energy of a disturbance of a given wave number are presented. Such equations, which include the effects of the generation and release of potential energy, friction, and the transfer of energy among the various scales of eddies and the mean flow, can serve as a basis for studying the day-to-day variations of the spectral distribution of kinetic energy and for computing the ?steady-state? atmospheric energy cycle in the domain of wave number, with the use of daily hemispheric data.
dc.publisherAmerican Meteorological Society
dc.titleEQUATIONS GOVERNING THE ENERGETICS OF THE LARGER SCALES OF ATMOSPHERIC TURBULENCE IN THE DOMAIN OF WAVE NUMBER
dc.typeJournal Paper
dc.journal.volume14
dc.journal.issue6
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1957)014<0513:EGTEOT>2.0.CO;2
dc.journal.fristpage513
dc.journal.lastpage523
dc.treeJournal of Meteorology:;1957:;volume( 014 ):;issue: 006
dc.contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record