Novel Wave Models and Diffusion Coefficients for Plasmaspheric Hiss and Low Frequency Hiss

The Earth's inner magnetosphere is populated by a host of high frequency plasma waves which, via wave-particle interactions, can shape the dynamics of the terrestrial radiation belts. One of these is an incoherent whistler-mode plasma wave commonly referred to as hiss. Hiss is nearly always present in the inner magnetosphere, acting to diffusively scatter electrons into the atmosphere. While hiss ...