“…The previous studies on the ballooning mode are important to shed light on substorm physics, particularly the triggering process of the impulsive magnetic events in the near‐Earth magnetosphere and auroral ionosphere, as well as the low‐frequency oscillations in the plasma sheet generated by some impulsive source at the center of the magnetotail, propagating toward both dawn and dusk. Nevertheless, as pointed out by Mazur et al [], the exact expressions of the dispersion equation derived by different pioneer authors happened to be somewhat different from each other [e.g., among those provided by Safargaleev and Maltsev , , Ohtani and Tamao , , and Liu , ]. More seriously, these theoretical analysis of the ballooning instability encountered difficulties to recover the basic shear Alfvén mode and the magnetosonic mode in uniform, ideal plasmas, namely [e.g., Boyd and Sanderson , ; Bellan , ], and the fundamental ballooning mode in incompressible plasmas, namely [e.g., Kadomtsev , ; Mikhailovskii , ; Hirose et al , ; Hirose and Joiner , ], where in equations and , ω is the wave frequency, c A and c s are the Alfvén and sound speeds, respectively, k and k z are the total and the parallel wave numbers, respectively, γ and β are the adiabatic index and plasma beta number, respectively, k p and k c are the averaged inverse scale length of the pr...…”