“…Similarly, during a recovery phase of a storm, the newly trapped electrons can be transported inwards and thus accelerated by the ULF waves (e.g., Ozeke et al., 2020; Silva et al., 2022) or accelerated locally due to the interaction with hiss (e.g., J. Li et al., 2019) or chorus waves (e.g., Horne et al., 2005; Hua et al., 2022). Lower energy electrons (1–10s keV) are also often impacted by the presence of kinetic Alfven waves in the auroral regions of the magnetosphere (see, e.g., review by Lysak (2023), and references within). These processes are often referred to as radiation belt “acceleration” or “enhancement” (see, e.g., review by Millan and Baker (2012)).…”