These foreshock transients are characterized by a core region with field strength decrease, density decrease, temperature increase, and flow deflection, on a spatial scale of a few R E (see review by Eastwood et al. (2005), Facskó et al. (2010), and Zhang et al. ( 2022)). Because the dynamic pressure inside them is extremely low, they can cause the local bow shock and magnetopause to move outward, leading to disturbances in the magnetosphere and ionosphere, including magnetospheric ULF waves, field aligned currents, traveling convection vortices, and auroral brightening (e.g.,