The first research flights with an upward-pointing airborne lidar were conducted by Kwon et al. (1990) andHostetler et al. (1991) who computed horizontal and vertical wavenumber spectra between 80 and 100 km altitude from measurements acquired with an airborne Na lidar. Hostetler and Gardner (1994) combined Rayleigh and Na lidar observations to cover altitudes from 25 to 40 km and 80-105 km while Rayleigh lidar observations from Gao and Meriwether (1998) ranged from 30 to 45 km. All the findings from these early airborne lidar studies have in common that their horizontal wavenumber spectra in the troposphere, stratosphere and upper mesosphere support gravity waves (GW) as the underlying dynamical process for determining the horizontal wavenumber dependence in the mesoscale range.The mesoscale dynamics are characterized by horizontally rotational and horizontally divergent modes. In theoretical work it has been argued that the horizontal wavenumber dependence can be described by stratified turbulence associated with a forward inertial energy cascade (