“…EMIC waves are known to be generated by the cyclotron instability of anisotropic distribution of ∼10–100 keV ring current protons (e.g., Anderson et al., 1996; Chen et al., 2010; Cornwall, 1965; Meredith et al., 2014; Min et al., 2015; Saikin et al., 2015; Wang et al., 2016; Yue et al., 2019; Zhang et al., 2014). Cyclotron resonant interactions with EMIC waves are recognized to be one of the dominant mechanisms accounting for the rapid precipitation loss of radiation belt electrons (e.g., Aseev et al., 2017; Cao et al., 2020; Kersten et al., 2014; Liu et al., 2012, 2010; Meredith et al., 2003; Ni et al., 2015, 2018; Ni, Zhang, & Gu, 2022; Shprits et al., 2008, 2013, 2016, 2017; Summers et al., 2007; Summers & Thorne, 2003; Thorne & Kennel, 1971; Usanova et al., 2014; Zhang et al., 2016) and ring current protons (e.g., Bortnik et al., 2006; Cao et al., 2013, 2017, 2019; Cornwall et al., 1970; Jordanova et al., 2001; Lyons & Thorne, 1972; Ma et al., 2019; Millan & Thorne, 2007; Ni, Hua, et al., 2022; Usanova, 2021; Usanova et al., 2010; Xiao et al., 2011) into the atmosphere. EMIC waves can also heat thermal electrons and heavy ions (He + and O + ; e.g., Horne & Thorne, 1997; Thorne & Horne, 1997; Zhang et al., 2011; Zhu et al., 2021).…”