Dispersion imposed limits on atmospheric gravity waves in the mesosphere: Observations from OH airglow.

Mesospheric airglow perturbations offer a method of-observing fast (long ve rtical wavelengths, lambda(z) and short horizontal wavelengths, lambda(h)) atmospheric gravity waves (AGWs) propagating through the mesosphere. In a r ecent study, wave phase speeds (and lambda(h)) have been deduced from the a irglow observations and Doppler corrected using lidar winds [Swenson et al. , 1999]. Combining these measurements:with the dispersion relationship, wav e momentum and energy fluxes were calculated. The observed waves have intri nsic phase speeds which are not linearly related to lambda(z) for short lam bda(h) as is assumed in the commonly applied approximation to the dispersio n relation. This corrected dispersion relationship is graphically presented along with imager measurements of AGWs and an estimate of error in the wav e momentum flux related to this term. The observed waves with lambda(h) < 2 0 km are found to be near the high-frequency limit for vertical propagation , suggesting they may be ducted, evanescent, or close to the point of total internal reflection.