Journal ArticleDOI
Transient Response to Localized Episodic Heating in the Tropics. Part II: Far-Field Behavior.
Rolando R. Garcia,Murry L. Salby +1 more
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In this paper, the authors examined how these disturbances are modified as they propagate through the far field in the presence of spatially-varying background states, which can still be understood in terms of projection and barotropic components of the response.Abstract:
In Part I of this investigation, we described the stochastic, near-field behavior of disturbances excited by randomly evolving tropical heating. In the present paper, we examine how these disturbances are modified as they propagate through the far field in the presence of spatially-varying background states. Although the behavior can no longer be broken down into individual Hough modes, it can still be understood in terms of projection and barotropic components of the response. Responses to fast heating, as may be produced by daily fluctuations in convection, and to slow heating, evolving over seasonal time scales, are studied separately. For fast heating the projection response consists mainly of a spectrum of Kelvin waves which, in the lower stratosphere, is centered at frequencies corresponding to twice the effective depth of the heating. The spectrum shifts to higher frequency with increasing altitude due to differential damping. As a result, the slow, fast and ultrafast Kelvin waves identifi...read more
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Journal ArticleDOI
Gravity wave dynamics and effects in the middle atmosphere
TL;DR: In this article, a review of gravity wave sources and characteristics, the evolution of the gravity wave spectrum with altitude and with variations of wind and stability, the character and implications of observed climatologies, and the wave interaction and instability processes that constrain wave amplitudes and spectral shape are discussed.
Journal ArticleDOI
Convectively Coupled Equatorial Waves: Analysis of Clouds and Temperature in the Wavenumber–Frequency Domain
TL;DR: In this article, a wavenumber-frequency spectrum analysis is performed for all longitudes in the domain 158S−158N using a long (;18 years) twice-daily record of satellite-observed outgoing longwave radiation (OLR), a good proxy for deep tropical convection.
Journal ArticleDOI
Convectively-coupled equatorial waves
TL;DR: In this paper, the authors used convectively coupled equatorial waves (CCEWs) to simulate tropical rainfall variability in the equatorial beta plane of a tropical weather system, and found that CCEWs display a large degree of self-similarity over a surprisingly wide range of scales.
Journal ArticleDOI
Migrating and nonmigrating diurnal tides in the middle and upper atmosphere excited by tropospheric latent heat release
Maura E. Hagan,Jeffrey M. Forbes +1 more
TL;DR: In this paper, the global scale wave model (GSWM) is used to investigate mesospheric and lower thermospheric migrating and non-migrating diurnal tidal components that propagate upward from the troposphere, where they are excited by latent heat release associated with deep tropical convection.
Journal ArticleDOI
Large-Scale Dynamical Fields Associated with Convectively Coupled Equatorial Waves
TL;DR: In this paper, a linear regression between selectively filtered satellite-observed outgoing longwave radiation (OLR) data, and various fields from a global reanalysis dataset was used to isolate the convective variations contributing to spectral peaks that lie along the equatorial wave dispersion curves for equivalent depths in the range of 12-50 m.
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