Parametric modelling of density perturbation measurements obtained with the
University of Western Ontario's Purple Crow Lidar on 5 nights are used to
infer that the typical vertical wavenumber spectrum in the upper stratosphe
re is dominated by a few quasi-monochromatic waves. In general only 2 of th
ese waves, with growth or decay rates on the order of 1/(14 km) or less, ca
rry most of the spectral energy. These waves are present about half the tim
e on the nights studied. When analyzed using classical spectral techniques
these waves appear to form a continuous spectrum. These results may help ex
plain why general circulation models obtain reasonable climatologies when g
ravity wave parameterization schemes based on a small number of propagating
gravity waves are employed.