Abstract
Internal waves propagating through a dissipative fluid interact with the mean flow. In response to forcing by a single wave, the mean flow evolves to a steady solution. In the presence of two (or more) waves such a solution exists but is unstable. The underlying dynamics in the latter case are basically those discussed by Holton and Lindzen (1972) in their theory of the quasi-biennial oscillation. If viscosity is small but nonzero the zonal flow exhibits a long-period oscillation.
This study elucidates the dependence of the period and structure of the oscillation on the imposed parameters, and clarifies the basic dynamics. In particular, the origin of the downward motion of shear zones is discussed in detail following a demonstration (under realistic assumptions) that anomalies in the mean flow structure cannot propagate downward. Thus it is shown that the increase of radiative cooling coefficient with height in the stratosphere is not crucial to the mechanism while the mesospheric semi-annual oscillation is irrelevant for practical purposes. It is also argued that momentum diffusion in the lower stratosphere may be of crucial importance in the momentum budget of the oscillation.
