"Numerical simulation of a ducted gravity wave event suggests that OH (8,3) and O(1S) 557.7 nm airglow emissions layers may exhibit opposite-phase intensities when perturbed by a short-period wave undergoing vertical reflection. This effect arises due to the time and temperature dependance of the OH excitation reaction, coupled with the linear polarization properties of vertically-standing waves."
Geophysical Research Letters
American Geophysical Union
Scholarly Commons Citation
Snively, J. B., & Pasko, V. P. (2005). Antiphase OH and OI Airglow Emissions Induced By a Short-Period Ducted Gravity Wave. Geophysical Research Letters, 32(8). https://doi.org/10.1029/2004GL022221