Rg. Stockwell et Rp. Lowe, Airglow imaging of gravity waves 1. Results from a small network of OH nightglow scanning imagers, J GEO RES-A, 106(D15), 2001, pp. 17185-17203
Images of the variations of OH nightglow intensities have been recorded by
a three-station network of scanning radiometers in southwestern Ontario dur
ing the period from May until September 1998. Each radiometer performs a 16
by 16 point raster scan of the night sky every minute, turning itself on a
nd off when the solar depression angle is < 6 degrees. The horizontal phase
velocity, horizontal wavelength, and frequency of the internal gravity wav
es are derived from the OH intensity measurements using joint time-frequenc
y analysis techniques, including the S transform, localized cross-spectral
analysis, and generalized instantaneous frequency. The ensemble of gravity
waves seen in all three instruments are analyzed and observed to have a str
ong dependence in their propagation direction with the majority of waves se
en at each of the three sites having a horizontal wave vector in the northe
ast direction. The most common parameters observed for horizontal phase spe
ed is 45 m/s, horizontal wavelength is 25 km, and period is 10 min.