Fluctuations in the magnetic and electric fields result in diffusive motion of radiation belt electrons across Roederer's L* parameter (Fälthammar, 1965;Roederer, 1970), a version of the third adiabatic invariant. L* diffusion (henceforth referred to as radial diffusion) occurs at constant first and second adiabatic invariants, and the electron's energy is increased (reduced) with diffusion into regions of stronger (weaker) magnetic field. Much of the dynamics of the radiation belts can be attributed to radial diffusion and the subsequent energy change of the electron populations (Shprits et al., 2008), so understanding the rate of the diffusion is a vital factor for accurately predicting and reconstructing the evolution of electron populations.The primary origin of electric and magnetic fluctuations, driving radial diffusion, is widely accepted to be ultra-low frequency (ULF) wave activity (Elkington et al., 1999) in the Pc-5 band (1.67-6.67 mHz (Jacobs et al., 1964)). Wave-particle interactions between these ULF waves and radiation belt electrons are particularly effective when the wave frequency is a multiple of the electron drift frequency, constituting a drift-resonant interaction. If interactions with Pc-5 waves continue over a broad frequency range, then the displacement of a particle in L* may evolve stochastically, following continuous interactions with multiple waves, and be described as a diffusive process (Ukhorskiy & Sitnov, 2013;Ukhorskiy et al., 2009). In this diffusive regime, the radial diffusion coefficient, D LL , quantifies the mean square displacement of electrons across L*, and is a measure of the radial diffusion rate.