The complex structure inherent to frequently observed atmospheric gravity wave (GW) gatherings constitutes a challenge that remains difficult to address (e.g.,

Gravity waves (GWs) and the large-scale planetary waves and tides are the main drivers for the general circulation of the middle atmosphere. The primary sources of GW are topography, convection, fronts, instabilities, and spontaneous adjustment (e.g., Fritts & Alexander, 2003). GW constitute an important dynamical coupling mechanism between different regions and layers of the atmosphere by redistributing energy and momentum over

Gravity waves (GWs) and the large-scale planetary waves and tides are the main drivers for the general circulation of the middle atmosphere. The primary sources of GW are topography, convection, fronts, instabilities, and spontaneous adjustment (e.g., Fritts & Alexander, 2003). GW constitute an important dynamical coupling mechanism between different regions and layers of the atmosphere by redistributing energy and momentum over