Pi2 pulsations, with periods in the range of 40-150 s (Jacobs et al., 1964), are an ultralow-frequency (ULF) phenomenon associated with magnetospheric substorms and other disturbances originating in the near-Earth magnetotail (Keiling & Takahashi, 2011;Olson, 1999;Saito et al., 1976). Ground magnetometers located at low latitudes (L <2) detect Pi2 pulsations at all local times (Nosé, 1999), making the pulsations a valuable indicator of substorm onsets. The fact that low-latitude Pi2 pulsations exhibit nearly identical waveforms at different local times (Tokunaga et al., 2007;Yumoto et al., 1990) implies that the source oscillations in the magnetosphere have a large spatial coherence length. There are two possible mechanisms for establishing the global oscillations in the magnetosphere. One is generation of propagating fast mode waves by braking of bursty bulk flows that already have a Pi2 periodicity (Kepko et al., 2001). The other is excitation of plasmaspheric cavity mode resonance (Yeoman & Orr, 1989) or virtual resonance (Lee, 1998) by impulsive or broadband disturbances generated in the near-Earth magnetotail. These resonances both exhibit discrete frequencies and eigenmode structures, so we will hereinafter refer to both of them as cavity mode. The disturbances can be bursty bulk flows with random periodicity. Previous statistical studies using satellite data found radially standing structures of compressional Pi2 waves in the inner magnetosphere, in favor of the cavity mode interpretation (Park et al., 2020;