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dc.contributor.authorPlatzman, George W.
dc.date.accessioned2017-06-09T14:12:29Z
dc.date.available2017-06-09T14:12:29Z
dc.date.copyright1960/12/01
dc.date.issued1960
dc.identifier.issn0095-9634
dc.identifier.otherams-14679.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150266
dc.description.abstractThe nonlinear aspects of the vorticity equation for two-dimensional planetary circulations of the earth's atmosphere may be studied by expansion of the solution in spherical surface harmonics. Some of the main mathematical problems are discussed here that arise in an examination of the ?spectral? form of the vorticity equation which results from such an expansion. The truncation of the spectral equations is discussed, and a proof is given of the invariance of mean square velocity and vorticity for truncated spectra. Some comments are made on low-order systems, which are to be followed by a detailed investigation of three-component systems in the second part of this study.
dc.publisherAmerican Meteorological Society
dc.titleTHE SPECTRAL FORM OF THE VORTICITY EQUATION
dc.typeJournal Paper
dc.journal.volume17
dc.journal.issue6
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1960)017<0635:TSFOTV>2.0.CO;2
dc.journal.fristpage635
dc.journal.lastpage644
dc.treeJournal of Meteorology:;1960:;volume( 017 ):;issue: 006
dc.contenttypeFulltext


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