Man-made very low frequency (VLF) waves and naturally generated plasma waves are frequently observed in the Earth's inner radiation belt (L ∼ 1.2-2) and slot region (L ∼ 2-3). Man-made VLF waves (tens of kHz) come from ground-based transmitters (Clilverd et al., 2008;Helliwell & Katsufrakis, 1974;Zhao et al., 2019) or spaceborne transmitters such as the Demonstration and Science Experiments (DSX) satellite (Scherbarth et al., 2009). Natural plasma waves cover a wide band from extremely low frequency (ELF) to VLF, including lightning-generated whistlers (LGWs) and plasmaspheric hiss and so on. LGWs (f ∼ 100-10 kHz) are injected from the troposphere after lightning strikes (Inan et al., 2007;Záhlava et al., 2019). Plasmaspheric hiss (f ∼ 20-4000 Hz) may be excited by the anisotropic instability of hot electrons (Chen et al., 2012) or originates from the inward penetration of whistler-mode chorus waves (Bortnik et al., 2009). The hiss intensity depends on solar wind dynamic pressure, plasma flow velocity, orientation of interplanetary magnetic field (IMF) (L.