Ubiquitous throughout the universe, shocks form when a supersonic flow encounters an obstacle and are important particle accelerators through different acceleration mechanisms (e.g., Helder et al., 2012;Lee et al., 2012). On Earth, a bow shock forms when the supermagnetosonic solar wind encounters the magnetosphere. At the quasi-parallel bow shock (where the angle between the shock normal and the interplanetary magnetic field (IMF) is less than 45°), some solar wind particles are reflected by the bow shock and populate the region upstream known as the foreshock (e.g., Eastwood et al., 2005). Interactions between these foreshock particles and the incoming solar wind particles can generate ULF waves that permeate the foreshock (e.g., Eastwood et al., 2005;Wilson et al., 2016). In addition, transient kinetic phenomena are also observed in the foreshock (see review by Zhang et al., 2022), such as hot flow anomalies (HFAs) (