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Titlebook: Coupling Processes in the Lower and Middle Atmosphere; Eivind V. Thrane,Tom A. Blix,David C. Fritts Book 1993 Springer Science+Business Me

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Convectively Generated Stratospheric Gravity Waves: The Role of Mean Wind Shear of momentum into the stratosphere. Cases with and without stratospheric mean wind shear are compared. In the latter case Doppler shifting of the waves to lower frequencies leads to wave breaking and enhanced wave — mean-flow interaction.
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Der Einfluss von Kultur auf die Wirtschaft,een the reversible and the irreversible cases at a critical amplitude of the wave forcing. The evolution is highly dependent on the latitudinal profile of the initial mean zonal wind; if the mean zonal wind is symmetric with respect to the equator, the vortex breaks easily, while it is very robust for anti-symmetric mean zonal winds.
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Nonlinear Evolution of an Upward Propagating Gravity Wave: A Numerical Case Studyh height approximately as if the wave had reached saturation, even prior to breakdown. Therefore, observations of limited wave growth with height may reflect the natural and gradual nonlinear evolution of upward propagating gravity waves before breakdown.
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