“…There are explosive events that created a broad spectrum of perturbations in both acoustic and gravity wave modes, for example, rocket launches that produce shock‐acoustic waves followed by concentric gravity waves (Lin, Shen, et al., 2017) or thermospheric ducted gravity waves (M.‐Y. Chou et al., 2018). An extreme case is the 2011 Tohoku earthquake and tsunami, which triggered diverse spectra of TIDs with phase velocities of ∼3.5 km/s (Rayleigh wave), 1–1.2 km/s (acoustic wave), ∼300–590 m/s (gravity wave), and ∼200–250 m/s (tsunami wave) (e.g., Azeem et al., 2017; Chen et al., 2011; M.‐Y.…”