Whistler waves are common upstream features of planetary bow shocks and are involved in shock formation and particle interactions (Balogh & Treumann, 2013;Oka et al., 2017Oka et al., , 2019. Two types of whistler waves emitting from shock ramps have been previously identified: propagating and phase standing (Russell & Farris, 1995). The propagation direction of propagating whistler waves has a small angle with respect to the magnetic field and they propagate far upstream (Russell, 2007). They have been widely observed upstream of the bow shock of Earth and are typically called "1 Hz" waves. Furthermore, they are also commonly observed in other planetary shocks,