“…Although ground‐based airglow observations can be interrupted by local weather conditions, they contribute significantly to the understanding of EPB evolution and the associated physical processes. Ground‐based all‐sky airglow imagers have been previously used to investigate the morphological features of EPBs, including seasonal and daily variations of occurrence rates [ Sahai et al ., ; Makela et al ., ; Nade et al ., ; Sharma et al ., ], their zonal drift velocities [ Martinis et al ., ; Pimenta et al ., ; Yao and Makela , ; Pautet et al ., ; England and Immel , ; Nade et al ., ; Sharma et al ., ], poleward extensions or apex height changes [ Sahai et al ., , , ; Kelley et al ., ], the distance (or spacing) changes between adjacent EPB depletions in a group of EPBs [ Makela et al ., ], bifurcation and tilt of EPBs [ Weber et al ., ; Anderson and Mendillo , ; Mendillo and Tyler , ; Sinha and Raizada , ], and influences of geomagnetic and solar activities [ Sahai et al ., ; Yao and Makela , ]. All of these studies cited here, however, were made in North America, Brazil, and India regions.…”