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contributor authorMcIntyre, M. E.
contributor authorWeissman, M. A.
date accessioned2017-06-09T14:20:12Z
date available2017-06-09T14:20:12Z
date copyright1978/07/01
date issued1978
identifier issn0022-4928
identifier otherams-17507.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153409
description abstractShear instabilities can result in waves being radiated far from the seat of instability. This phenomenon, and its opposite extreme, the trapping of instabilities, can be described and interdistinguished by linear theory for slowly growing instabilities only. To describe strong instabilities which radiate, laboratory and numerical studies are needed. Linear theory can better describe the somewhat similar phenomenon of ?resonant overreflection,? which for a constant incident wave is characterized by linear rather than exponential growth in fine. The energy budget of sustained radiation, or overreflection, from a shear layer does not necessarily involve net removal of energy from the neighborhood of the shear layer.
publisherAmerican Meteorological Society
titleOn Radiating Instabilities and Resonant Overreflection
typeJournal Paper
journal volume35
journal issue7
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1978)035<1190:ORIARO>2.0.CO;2
journal fristpage1190
journal lastpage1196
treeJournal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 007
contenttypeFulltext


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