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Experimental Constraints on Gravity Wave Parameterization from in Situ Measurements of Temperature on of gravity wave breaking in models. The meridional temperature reversal and the very cold mesopause temperatures in summer of ~130 K have put a serious constraint on any theoretical description of the physical processes acting in the upper atmosphere. In this paper mesospheric temperature measure

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On the nonlinear interactions between gravity waves in shear flows,ve instability. When they are strictly isolated, they can be satisfactorily described by the linear theory because of the (almost) incompressibility of the atmosphere. In general, however, several waves coexist, and the nonlinear interactions can significantly influence their propagation far below t