“…The inner magnetosphere is a highly dynamic and complex system with various populations (including the coexisting and overlapping cold plasmasphere, energetic ring current, and relativistic radiation belt particles), which are governed by the time varying electric and magnetic fields (e.g., Yue, Bortnik, Chen, et al., 2017; Yue, Bortnik, Thorne, et al., 2017; Yue et al., 2016, 2018, 2019). Especially, ions with energy from 1 to 20 keV are strongly affected by the competition between electric field drifts and the magnetic gradient and curvature drifts, which may generate different type of ions spectral structures, such as “nose‐like” structures (e.g., Buzulukova et al., 2003; Ebihara et al., 2004; Fennell et al., 1998; Ferradas et al., 2016a, 2016b; Ganushkina et al., 2001; Li et al., 2000; Smith & Hoffman, 1974; Vallat et al., 2007), “wedge‐like” dispersions (e.g., Ebihara et al., 2001; Ren et al., 2020, 2021; Yamauchi et al., 2006; Zhou et al., 2020), “trunk‐like” structures (Zhang et al., 2015), low‐energy “finger” (e.g., Wang et al., 2020), and ion spectral gaps or stagnation dips (e.g., Buzulukova et al., 2002; Fennell et al., 1981; Kaye et al., 1981; Kistler & Mouikis, 2016; Kistler et al., 1989; Kovrazhkin et al., 1999; Lennartsson et al., 1979; Shirai et al., 1997; Yue et al., 2021).…”