A NOTE ON OVERSTABILITY AND THE ELASTOID-INERTIA OSCILLATIONS OF KELVIN, SOLBERG, AND BJERKNES

dc.contributor.author	Fultz, D.
dc.date.accessioned	2017-06-09T14:12:05Z
dc.date.available	2017-06-09T14:12:05Z
dc.date.copyright	1959/04/01
dc.date.issued	1959
dc.identifier.issn	0095-9634
dc.identifier.other	ams-14511.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4150081
dc.description.abstract	Results elucidating the mechanism by which overstable (oscillating) cellular convection occurs in rotating layers are given. There is a close connection with the elastoid-inertia oscillations in a rotating cylinder discussed by Kelvin, Solberg, and Bjerknes, and it is found that diffusion of heat by conduction acts in a deslabilizing way in the motion. Simple experiments in a rotating cylinder on the elastoid-inertia oscillations show a remarkably close agreement with the free periods calculated theoretically. This, in the field of meteorological experiments, is important in establishing close agreement with meteorological theory in a situation where the flow can be strongly ageostrophic.
dc.publisher	American Meteorological Society
dc.title	A NOTE ON OVERSTABILITY AND THE ELASTOID-INERTIA OSCILLATIONS OF KELVIN, SOLBERG, AND BJERKNES
dc.type	Journal Paper
dc.journal.volume	16
dc.journal.issue	2
dc.journal.title	Journal of Meteorology
dc.identifier.doi	10.1175/1520-0469(1959)016<0199:ANOOAT>2.0.CO;2
dc.journal.fristpage	199
dc.journal.lastpage	208
dc.tree	Journal of Meteorology:;1959:;volume( 016 ):;issue: 002
dc.contenttype	Fulltext