Non-Singular Resonance of Equatorial Waves Under the Radiation ConditionSource: Journal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 002::page 183Author:Hayashi, Yoshikazu
DOI: 10.1175/1520-0469(1976)033<0183:NSROEW>2.0.CO;2Publisher: American Meteorological Society
Abstract: A 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.
|
Collections
Show full item record
contributor author | Hayashi, Yoshikazu | |
date accessioned | 2017-06-09T14:18:40Z | |
date available | 2017-06-09T14:18:40Z | |
date copyright | 1976/02/01 | |
date issued | 1976 | |
identifier issn | 0022-4928 | |
identifier other | ams-16990.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4152834 | |
description abstract | A 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. | |
publisher | American Meteorological Society | |
title | Non-Singular Resonance of Equatorial Waves Under the Radiation Condition | |
type | Journal Paper | |
journal volume | 33 | |
journal issue | 2 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1976)033<0183:NSROEW>2.0.CO;2 | |
journal fristpage | 183 | |
journal lastpage | 201 | |
tree | Journal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 002 | |
contenttype | Fulltext |