Plasmaspheric hiss is one kind of structureless broadband whistler mode wave with a frequency ranging from 20 Hz to 2 kHz (Tsurutani et al., 2015). The hiss wave is typically identified in the plasmasphere and the plasmaspheric plume (W. . It takes on a critical significance in the loss of 100 keV-1 MeV electrons from the Earth's radiation belts due to pitch angle scattering (Ma, Li, Thorne, Bortnik, et al., 2016), thus playing a major role in forming a slot region between the inner and outer electron belts (Lyons et al., 1972). In general, the estimates of the global radiation belt electron loss time scale due to hiss waves are calculated using a quasi-linear diffusion model (