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contributor authorHayashi, Yoshikazu
date accessioned2017-06-09T14:18:40Z
date available2017-06-09T14:18:40Z
date copyright1976/02/01
date issued1976
identifier issn0022-4928
identifier otherams-16990.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152834
description abstractA response of large-scale equatorial waves to a thermal or a lateral forcing confined in the troposphere is examined analytically by imposing. the radiation condition based on an equatorial beta-plane model without wind shear. A resonant response with large finite amplitude occurs under the radiation condition, when the vertical scale of the wave coincides with that of the forcing. This ?non-singular resonance? is associated with a sharp spectral peak for equatorial waves which are characterized by a small variation of the frequency with the vertical wavenumber. However, such resonant equatorial waves are not realistic, since their vertical velocity is not in phase with the imposed convective heating and their pressure is not in geostrophic balance with the meridional wind of the imposed mid-latitude disturbances. This study suggests that the forcing cannot be imposed arbitrarily regardless of its feedback. It assures on the other hand that the equatorial waves simulated by a general circulation model are not spurious resonant waves resulting from an artificial reflection at the top of a finite-difference model.
publisherAmerican Meteorological Society
titleNon-Singular Resonance of Equatorial Waves Under the Radiation Condition
typeJournal Paper
journal volume33
journal issue2
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1976)033<0183:NSROEW>2.0.CO;2
journal fristpage183
journal lastpage201
treeJournal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 002
contenttypeFulltext


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