Numerical simulations demonstrate theoretical predictions that gravity waves with short periods (∼4–8 min) in the mesosphere and lower thermosphere may force secondary acoustic waves, with harmonic periods (∼2-4 minutes), that can reach detectable amplitudes in the thermosphere and ionosphere. The mechanism is through their vertical fluxes of vertical momentum, which lead to forcing as they are disrupted by varying stratification or instability. This is shown likely to occur where horizontally or radially opposing gravity waves interact at large amplitudes, such as above large convective sources, and after overturning. Evanescence and reflection of the waves can lead to further enhancements of the vertical fluxes and the potential for forcing. Results thus identify one of likely several mechanisms for the nonlinear conversion from gravity waves to acoustic waves, to elucidate an unappreciated source of vertical coupling.
Geophysical Research Letters
American Geophysical Union
Scholarly Commons Citation
Snively, J. B. (2017). Nonlinear Gravy Wave Forcing as a Source of Acoustic Waves in the Mesosphere, Thermosphere, and Ionosphere. Geophysical Research Letters, 44(3). https://doi.org/10.1002/2017GL075360
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