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contributor authorBoville, Byron A.
date accessioned2017-06-09T14:22:11Z
date available2017-06-09T14:22:11Z
date copyright1981/03/01
date issued1981
identifier issn0022-4928
identifier otherams-18107.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154076
description abstractAmplitude vacillation is studied using a spectral version of the two-level quasi-geostrophic model in a ?-plane channel. The parameters are chosen so that only a single wave may be unstable to the undisturbed basic state. It is shown that the weakly nonlinear theories which have been proposed do not work well on the ?-plane, because nonlinear interactions are not negligible even though only a single wave has any significant amplitude. The energetics and mechanism of amplitude vacillation on a ?-plane are discussed for a case with moderate dissipation and contrasted with the mechanism on an f-plane.
publisherAmerican Meteorological Society
titleAmplitude Vacillation on a β-Plane
typeJournal Paper
journal volume38
journal issue3
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1981)038<0609:AVOAP>2.0.CO;2
journal fristpage609
journal lastpage618
treeJournal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 003
contenttypeFulltext


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