Whistler-mode chorus emissions with rising-tone and falling-tone frequencies have been studied for more than half a century. Chorus emissions are often observed outside the plasmapause in conjunction with magnetospheric substorms (Tsurutani & Smith, 1974). Chorus emissions are essentially nonlinear phenomena induced by finite amplitude waves as evidenced by the triggered emissions from the VLF transmitters, which exhibit the same frequency spectra with varying frequencies (see a review by Omura et al., 1991;Gołkowski et al., 2019). Recently, demonstration and science experiments (DSX;Scherbarth et al., 2009) was conducted for the study of whistler-mode wave-particle interactions. They injected whistler-mode wave to trigger new emissions in the magnetosphere. Propagation characteristics of the DSX waves have been studied base on ray-tracing (Reid et al., 2021). Chorus is an emission triggered by a naturally growing wave at a fixed frequency as predicted by linear growth rates (Kennel & Petschek, 1966). From the electromagnetic thermal fluctuations, a wave with the maximum linear growth rate grows to the largest amplitude, and it suppresses growth of other waves with frequencies close to its frequency through scattering of resonant electrons. The wave becomes coherent and works as a triggering wave we assume in the present study. Under a finite amplitude coherent wave, resonant electrons undergo nonlinear motion and form either an electron hole or a hill, inducing resonant currents. The resonant currents cause variation of the wave amplitude and frequency as described by the wave equations (Nunn, 1974;Omura et al., 1991Omura et al., , 2008Vomvoridis et al., 1982). A wave with a frequency different from that of the triggering wave is generated as a wave packet independent from the triggering wave. The evolution of the newly generated wave packet has not been understood completely. It has been reported that series of short wave packets are generated sequentially, forming rising and/or falling-tone emissions. Each wave packet is called a subpacket of chorus elements (Foster et al., 2017;Santolík et al., 2014).
Subpacket structures of chorus waves have great importance on electron acceleration and pitch angle scattering.A simulation study has shown that efficient electron acceleration takes place by a finite packet via nonlinear electron trapping (Hiraga & Omura, 2020). Electron precipitations to the ionosphere due to chorus waves are observed by simultaneous observations between satellite and ground, which show the agreement with the pulsating aurora and each of chorus emissions with subpacket structure (Kasahara et al., 2018;Ozaki et al., 2018). A particle simulation of triggered emission (Hikishima et al., 2010) also showed that each triggered chorus element has subpacket structure and the electron flux is strongly modulated by the subpackets.The subpacket structure is also found in electromagnetic ion cyclotron (EMIC) rising-tone emissions (Nakamura et al., 2014). A model of the generation process of EMIC emissions...