The relation of gravity waves and turbulence in the mesosphere

VHF radar observations of the mesosphere generally reveal that the structure of turbulence is intermittent in space and time. Some examples of such turbulence layers and the concurrent gravity wave oscillations, observed in the low latitude mesosphere over the Arecibo Observatory/Puerto Rico are discussed. This turbulence structures which are intermittent on short time scales but persistently recur over periods of many hours at almost the same height are evidently not related to the simultaneously occurring short period gravity waves. These kinds of persistent turbulence structures are assumed to be related to very long period (inertia-) gravity waves, where instability takes place only by the wave induced shear in a narrow critical level. However, the short period gravity waves occasionally break into turbulence by overturning and convective instability. These interpretations offer a way to understand the generation mechanisms of the different kinds of turbulence structures, namely blobs, sheets and layers, which were reported in the early days of mesospheric VHF radar observations.