A nonlinear theory of internal gravity waves is extended to slowly varying mean winds u0. This theory determines the wave amplitudes, enhanced diffusion and momentum deposition, for a broad spectrum of waves as well as for a single wave. It is shown that the momentum deposition is not constant with altitude, even above the altitude where a wave saturates (breaks). The deposition is seen to decrease as a critical level is approached.-from Author
CITATION STYLE
Weinstock, J. (1982). Nonlinear theory of gravity waves: momentum deposition, generalized Rayleigh friction, and diffusion. Journal of the Atmospheric Sciences, 39(8), 1698–1710. https://doi.org/10.1175/1520-0469(1982)039<1698:NTOGWM>2.0.CO;2
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