R. Sica, and A. Russell. Geophysical Research Letters, 26 (24):
3617�3620(1999)
Abstract
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 stratosphere is dominated by a few quasi-monochromatic waves. In general only 2 of these waves, with growth or decay rates on the order of 1/(14 km) or less, carry most of the spectral energy. These waves are present about half the time on the nights studied. When analyzed using classical spectral techniques these waves appear to form a continuous spectrum. These results may help explain why general circulation models obtain reasonable climatologies when gravity wave parameterization schemes based on a small number of propagating gravity waves are employed.
%0 Journal Article
%1 p00420
%A Sica, RJ
%A Russell, AT
%D 1999
%J Geophysical Research Letters
%K imported sica
%N 24
%P 3617�3620
%T How many waves are in the gravity wave spectrum?
%V 26
%X 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 stratosphere is dominated by a few quasi-monochromatic waves. In general only 2 of these waves, with growth or decay rates on the order of 1/(14 km) or less, carry most of the spectral energy. These waves are present about half the time on the nights studied. When analyzed using classical spectral techniques these waves appear to form a continuous spectrum. These results may help explain why general circulation models obtain reasonable climatologies when gravity wave parameterization schemes based on a small number of propagating gravity waves are employed.
@article{p00420,
abstract = {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 stratosphere is dominated by a few quasi-monochromatic waves. In general only 2 of these waves, with growth or decay rates on the order of 1/(14 km) or less, carry most of the spectral energy. These waves are present about half the time on the nights studied. When analyzed using classical spectral techniques these waves appear to form a continuous spectrum. These results may help explain why general circulation models obtain reasonable climatologies when gravity wave parameterization schemes based on a small number of propagating gravity waves are employed.},
added-at = {2019-04-05T21:27:46.000+0200},
author = {Sica, RJ and Russell, AT},
biburl = {https://www.bibsonomy.org/bibtex/25872c4a3f7e21a52b2cab9dcded026d9/bobsica},
interhash = {53141d10c760567621405fb789b1206c},
intrahash = {5872c4a3f7e21a52b2cab9dcded026d9},
journal = {Geophysical Research Letters},
keywords = {imported sica},
location = {Univ Western Ontario, Dept Phys & Astron, London, ON N6A 3K7, Canada},
number = 24,
pages = {3617�3620},
timestamp = {2019-04-05T21:27:46.000+0200},
title = {How many waves are in the gravity wave spectrum?},
volume = 26,
year = 1999
}