“…Strong substorms with Kp ∼ 5–6 and AE ∼ 600–1,000 nT usually correspond to a time‐ and MLT‐averaged chorus wave power
pT 2 at latitudes λ ∼ 15° of cyclotron resonance with 100 keV electrons near the loss‐cone at L ∼ 5–6 (Agapitov et al.,
2018). To reduce the lifetime τ L to its minimum value, τ SD ( E min ) ∼ 140 s, the average wave power must increase up to
pT 2 , a level sometimes observed for hours at L ∼ 5 during geomagnetic storms and substorms (Chakraborty et al.,
2022; Elliott et al.,
2022; C. Tang et al.,
2023), or during microbursts (Zhang et al.,
2022). Such large amplitudes can lead to electron trapping and nonlinear acceleration (Katoh & Omura,
2007; Vainchtein et al.,
2018; Zhang et al.,
2019), but significant wave amplitude modulations and random phase jumps between and inside intense wave packets usually restore a diffusive‐like electron transport that can be approximated by quasi‐linear diffusion (Artemyev et al.,
2021,
2022; Z.…”