In space plasma physics, ULF waves play a significant role, for example, in coupling the solar wind, magnetosphere, and ionosphere. They also serve as a valuable diagnostic of coupling processes in the magnetosphere-ionosphere system. "Geomagnetic pulsations" is a general term for ULF waves observed on the ground. Jacobs et al. (1964) divided geomagnetic pulsations with frequencies less than 5 Hz into five regular and two irregular frequency bands. Quasi-sinusoidal waves are referred to as pulsation continuous (Pc), while irregular waveforms are referred to as pulsation irregular (Pi) (Arora et al., 2011). The three lower frequency bands of Pc waves (Pc3-5) are relevant to magnetospheric field line and cavity resonances (the subject of this paper), whereas internal wave-particle interactions generate the higher-frequency bands (