Background and MotivationUnderstanding, specification, and mitigation of the geomagnetically trapped radiation effects on human activity in space have been topics of intense interest since the discovery of the Van Allen belts in 1958, for example, Song et al. (2001). Concerns about damage to Earth-orbiting satellite systems and humans in space have led to studies of ways such threats may be mitigated through controlled precipitation of energetic electrons from the radiation belts (Kennel & Petschek, 1966). Loss of energetic electrons from the radiation belts is known to occur as a result of Doppler-shifted gyro-resonance interactions with in situ VLF, or physically, whistler-mode waves, examples being scattering by lightning-generated whistlers, magnetospheric activity-related whistler-triggered wave bursts, bursts of natural whistler-mode noise, and whistler-mode signals from high-power ground-based VLF communication transmitters (Abel & Thorne, 1998;Imhof et al., 1983). Here we note that the whistler mode may cover