“…Radiation belt electrons can be affected by various magnetospheric wave modes, including whistler mode chorus, plasmaspheric hiss, magnetosonic waves, electromagnetic ion cyclotron waves, and electrostatic electron cyclotron harmonic waves, via wave-particle interaction processes (e.g., Ni et al, 2016;Shprits et al, 2008;Summers et al, 2007;Thorne, 2010), and ultralow frequency wave-driven diffusion (e.g., Su, Zhu, Xiao, Zong, et al, 2015). Among these waves, hiss is typically regarded as a structureless, broadband whistler mode emission naturally occurring inside the plasmasphere (e.g., Meredith et al, 2004;Thorne et al, 1973), high-density plasmaspheric plumes (e.g., Summers et al, 2008;Zhang et al, 2018), and lowdensity plasmatrough (Hua et al, 2018;Su et al, 2018a;Zhu et al, 2015). A few recent studies reported hiss emissions with short-time (tens of milliseconds) rising and falling tones (Summers et al, 2014), long-lasting (~1 s) rising tones, and large amplitude (up to 1.5 nT) hiss waveforms in the plasmaspheric plumes (Su et al, 2018b).…”