“…An early attempt to model the effect of LGW on trapped electrons is Abel and Thorne (, Table 1), who assumed a constant LGW amplitude of B m = 10 pT and an occurrence rate of 3% to produce a drift LGW intensity of 3 pT 2 that is independent of location and geomagnetic activity. Other authors adjusted the LGW occurrence rate based on literature and/or empirical knowledge of observed electron flux decay (e.g., Drozdov et al, ; Kim et al, ; Ripoll, Chen, et al, ; Subbotin et al, ). An empirical database of LGW intensity has been produced as a function of L shell, magnetic local time, and geomagnetic activity (Figure 1 of Meredith et al, ).…”