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Gravity wave saturation in the middle atmosphere: A review of theory and observations

David C. Fritts
- 01 Aug 1984 - 
- Vol. 22, Iss: 3, pp 275-308
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TLDR
A review of recent advances in the understanding of gravity wave saturation in the middle atmosphere can be found in this article, where a brief discussion of the studies leading to the identification of the gravity wave effects and their role in middle atmosphere dynamics is presented.
Abstract
This paper provides a review of recent advances in our understanding of gravity wave saturation in the middle atmosphere. A brief discussion of those studies leading to the identification of gravity wave effects and their role in middle atmosphere dynamics is presented first. This is followed by a simple development of the linear saturation theory to illustrate the principal effects. Recent extensions to the linear saturation theory, including quasi-linear, nonlinear, and transient effects, are then described. Those studies addressing the role of gravity wave saturation in the mean circulation of the middle atmosphere are also discussed. Finally, observations of gravity wave motions, distribution, and variability and those measurements specifically addressing gravity wave saturation are reviewed.

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Citations
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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

Alleviation of a systematic westerly bias in general circulation and numerical weather prediction models through an orographic gravity wave drag parametrization

TL;DR: In this paper, the failure to parametrize subgrid-scale orographic gravity wave drag may account for the westerly biases in the northern hemisphere wintertime flow of the Meteorological Office 15-layer operational model and 11-layer general circulation model.
Journal ArticleDOI

The structure of the polar vortex

TL;DR: In this article, a comparative analysis of the 1987 Southern Hemisphere and 1989 Northern Hemisphere lower stratospheric, polar vortex circulation and constituent distributions as observed by the Airborne Antarctic Ozone Experiment, August 17-September 22, 1987, and Airborne Arctic Stratospheric Expedition, January 3-February 19, 1989 aircraft campaigns is presented.
Journal ArticleDOI

Measurement of turbulent energy dissipation rates in the middle atmosphere by radar techniques: A review

Wayne K. Hocking
- 01 Nov 1985 - 
TL;DR: In this article, the effects of turbulence on the width of signal spectra received by these radars are discussed, and it is shown how turbulence intensities may be extracted from spectral width measurements.
Journal ArticleDOI

INTERNAL GRAVITY WAVES: From Instabilities to Turbulence

TL;DR: In this paper, the authors review the mechanisms of steepening and breaking for internal gravity waves in a continuous density stratification and discuss the influence of those processes upon the fluid medium by mean flow changes.
References
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Journal ArticleDOI

Turbulence and stress owing to gravity wave and tidal breakdown

TL;DR: In this article, the effects of mean winds and gravity waves on the mean momentum budget were investigated and it was shown that the existence of critical levels in the mesosphere significantly limits the ability of gravity waves to generate turbulence.
Journal ArticleDOI

Internal atmospheric gravity waves at ionospheric heights

TL;DR: In this paper, the proper interpretation of irregular motions in the upper atmosphere has been investigated by a variety of techniques, but their proper interpretation has yet to be established. But their proper meaning has not yet been established.
Journal ArticleDOI

Propagation of planetary‐scale disturbances from the lower into the upper atmosphere

TL;DR: In this paper, the authors investigated the possibility that a significant part of the energy of the planetary-wave disturbances of the troposphere may propagate into the upper atmosphere and found that the effective index of refraction for the planetary waves depends primarily on the distribution of the mean zonal wind with height.
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A Dynamical Model of the Stratospheric Sudden Warming

TL;DR: In this article, the authors discussed the dynamics of the stratosphere sudden warming phenomenon in terms of the interaction of vertically propagating planetary waves with zonal winds, and verified the model by numerical integrations of the adiabatic-geostrophic potential vorticity equation.
Journal ArticleDOI

Planetary Waves in Horizontal and Vertical Shear: The Generalized Eliassen-Palm Relation and the Mean Zonal Acceleration

TL;DR: In this article, a new generalization of the Eliassen-Palm relations is proposed to study the zonal mean-flow tendency ∂ū/∂t due to waves in a stratified, rotating atmosphere with particular attention to equatorially trapped modes.
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