Atmospheric gravity waves (GWs) are small-scale propagating disturbances that arise due to the vertical forcing of air parcels by a disturbance in the flow. They are generated by a variety of meteorological processes, including flow over orography, atmospheric deep convection, and jet stream, cyclonic, and frontal instabilities. GWs play a wide range of key roles in the atmospheric system, particularly in the transfer of energy and momentum (e.g., Fritts & Alexander, 2003). They are responsible for driving the large-scale circulation in the middle atmosphere, primarily through accelerations to the mean-flow by the convergence of GW momentum flux (Fritts, 1984). They also modulate phenomena such as the Quasi-Biennial Oscillation