“…Particles show different behaviors at a quasi‐perpendicular shock and at a quasi‐parallel shock. At a quasi‐perpendicular shock, which has a distinguishable magnetic structure including foot, ramp and overshoot, a part of upstream incident particles can be reflected and quickly transmit into the downstream [ Leroy et al ., ; Sckopke et al ., ; Hada et al ., ; Lembège et al ., ; Ofman et al , ; Yang et al ., , , ; Guo and Giacalone , ; Ofman and Gedalin , ; Hao et al ., ; Gedalin , , , ; Johlander et al ., ; Tsubouchi et al ., ]; also, some reflected particles may travel along the background magnetic field to further upstream and lead to an ion foreshock [ Meziane et al ., ; Mazelle et al ., ; Savoini et al ., ]. At a quasi‐parallel shock, backstreaming particles generated by reflection can move far upstream along the background magnetic field, and then they will interact with upstream incident particles, resulting in the excitation of ultralow frequency (ULF) waves with oblique propagation [ Burgess , ; Scholer and Burgess , ; Lucek et al ., , , ; Tsubouchi and Lembège , ; Eastwood et al ., , ; Omidi et al ., , ; Wilson et al ., ; Shan et al ., , ; Wu et al ., ; Hao et al ., , ; Johlander et al ., ].…”