Cs. Gardner et al., OBSERVATIONS OF THE UNAMBIGUOUS 2-DIMENSIONAL HORIZONTAL WAVE-NUMBER SPECTRUM OF OH INTENSITY PERTURBATIONS, Geophysical research letters, 23(25), 1996, pp. 3739-3742
The unambiguous 2-D horizontal wave number spectrum of gravity wave pe
rturbations in OH emission intensities is computed from imager observa
tions acquired on 2 Feb 1995 at the Starfire Optical Range, NM. The te
chnique involves computing the (omega, k, l) = (omega, h, phi) spectru
m of OH images collected over a several hour period, where k is the zo
nal wave number, l is the meridional wave number, h = (k(2) + l(2))(1/
2), phi = tan(-1) (k/l), and omega is the temporal frequency. The data
are used to study the azimuthal distribution of wave energy propagati
on and the separability of the (h, phi) spectrum. The h spectral indic
es, computed from power-law fits of the 2-D spectrum over the wave num
ber range 2 pi/(200 km) < h < 2 pi/(20 km), vary between -1.6 and -3.6
as a function of phi with a mean of -2.58. Consequently, the image sp
ectrum is not separable in h and phi. We show that nonseparability is
most likely associated with distortion of the wave perturbations cause
d by the viewing geometry at large zenith angles.