The polar cap is defined as the area surrounded by the poleward boundary of auroral oval. The auroral arcs observed in the polar cap, called polar cap arcs (PCAs) for short, have been extensively studied. With the help of the global auroral imagers, some larger-scale PCAs, also referred to as transpolar arcs (TPAs), were noticed (e.g., Frank et al., 1982;Zhang et al., 2020;Zhu et al., 1997). According to different forms of evolution, the PCAs have been classified into different types, such as Sun-aligned arc (Berkey et al., 1976), theta aurora (Frank et al., 1986, and oval-aligned arc (Murphree & Cogger, 1981). Special attention is needed to distinguish the hook-shaped TPA and bending arcs. The former is Sun-aligned with a hook-shaped tailward arc (Ismail & Meng, 1982;Murphree et al., 1982). In contrast, the latter is a faint PCA splitting from the dayside auroral oval with anti-sunward moving (Kullen et al., 2015). These PCAs tend to occur during northward interplanetary magnetic field (IMF) with relatively quiet magnetic conditions (