“…Thus, electron interactions with waves are mostly modeled by solving the diffusion equation, which is mainly applicable in a strong background magnetic field, such as that of the near‐Earth magnetotail (Ni et al., 2016) and inner magnetosphere (see reviews by Li & Hudson, 2019; Shprits et al., 2008; Thorne et al., 2021 and references therein). Merging these two approaches (test particle simulations to follow adiabatic heating and solving the diffusion equation to track the effect of waves on the electron distributions) has been proposed, mostly for applications to the inner magnetosphere (e.g., Elkington et al., 2019; Lukin, Artemyev, & Petrukovich, 2021; Michael et al., 2021), but it has yet to be implemented.…”