Whistler waves are a type of electron-scale plasma waves that contribute to electron scattering, acceleration, and energy transport. Through wave-particle interactions, whistler waves shape the electron velocity distribution function. Properties of whistler waves can provide diagnostic information on the electron-scale physics in magnetic reconnection. Whistler waves have been intensively studied in magnetic reconnection (e.g., Khotyaintsev et al., 2019). Cluster observations in the magnetotail show that whistler waves have been observed prior to and during reconnection (Wei et al., 2007). In magnetotail reconnection whistler waves are frequently observed near the separatrix region and the magnetic pileup region (S. Y. Huang et al., 2017). In the pileup region, free energy for whistler waves comes from the temperature anisotropy (T e⊥ /T e‖ > 1) that results from betatron heating (