“…When observed in the meridian plane the oscillation appears to be standing. There is generally phase advance in the azimuthal direction, which is characterized by the azimuthal wave number m. Various sources have been identified such as Kelvin-Helmholtz oscillations at the magnetopause (Southwood, 1968), excitation of cavity or waveguide modes (Kivelson and Southwood, 1985;Samson et al, 1992), direct control by oscillations in the solar wind (Stephenson and Walker, 2002), and more recently fluctuating field-aligned currents in the auroral zone (Pilipenko et al, 2016). Pulsations can also be generated by drift-bounce resonance with ring current particles (Dungey, 1965).…”