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contributor authorPlatzman, George W.
date accessioned2017-06-09T14:12:29Z
date available2017-06-09T14:12:29Z
date copyright1960/12/01
date issued1960
identifier issn0095-9634
identifier otherams-14679.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150266
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.
publisherAmerican Meteorological Society
titleTHE SPECTRAL FORM OF THE VORTICITY EQUATION
typeJournal Paper
journal volume17
journal issue6
journal titleJournal of Meteorology
identifier doi10.1175/1520-0469(1960)017<0635:TSFOTV>2.0.CO;2
journal fristpage635
journal lastpage644
treeJournal of Meteorology:;1960:;volume( 017 ):;issue: 006
contenttypeFulltext


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