“…Once the distribution of wave intensity in geometrical space ( L ‐shell, MLT, and magnetic latitude) and the distribution of wave propagation angles are known, the local quasi‐linear diffusion coefficients can be calculated (Kennel & Engelmann, ; Lerche, ) and averaged over the 3‐D spatial domain of the radiation belts (e.g., Albert, ; Artemyev, Agapitov, et al, ; Horne et al, ; Glauert & Horne, ; Mourenas, Artemyev, Agapitov & Krasnoselskikh, ; Shprits & Ni, ). Such diffusion coefficients (expressed as functions of L ‐shell, MLT, and geomagnetic activity/solar wind conditions) are central to state‐of‐the‐art diffusion models describing radiation belt dynamics—that is, relativistic electron acceleration (e.g., Horne et al, ; Li et al, ; Mourenas et al, ; Thorne et al, ), electron precipitation (e.g., Ni et al, ; Thorne et al, ), and electron transport to lower L ‐shells (together with radial diffusion, e.g., Ma et al, ). Because a wide range of phenomena observed in the radiation belts can be described relatively successfully by quasi‐linear diffusion models (see also Albert et al, ; Drozdov et al, ; Glauert et al, ; Ma et al, ; Su et al, ), most past investigations of chorus waves have focused on the aforementioned wave parameters/characteristics needed to evaluate the quasi‐linear diffusion coefficients.…”