“…During magnetic activities, the observation of butterfly PAD can be located within L = 6 at all magnetic local time (MLT) [Lyons and Williams, 1975;Sibeck et al, 1987]. Currently, seven mechanisms have been proposed to explain the formation of the butterfly PAD during magnetic activities: (a) wave-particle interaction with magnetosonic waves and chorus waves [Horne et al, 2005a;Xiao et al, 2015;Li et al, 2016bLi et al, , 2016aChen et al, 2015;Maldonado et al, 2016], (b) nonlinear resonance with oblique electromagnetic ion cyclotron waves [Wang et al, 2016], (c) wave-particle interaction with hiss waves, lightening-generated whistlers and ground VLF transmitters [Albert et al, 2016], (d) outward adiabatic transports [Su et al, 2010], (e) magnetopause shadowing effect [e.g., Wilken et al, 1986], (f ) substorm injection combined with drift shell splitting [Sibeck et al, 1987], and (g) nonadiabatic scattering due to the field line curvature scattering [Artemyev et al, 2015] and adiabatic effect caused by ring current through the conservation of electron's magnetic moment [Lyons, 1977].…”