Wave-particle interactions play a crucial role in energetic particle dynamics in the Earth's radiation belts. However, the relative importance of different wave modes in these dynamics is poorly understood. Typically, this is assessed during geomagnetic storms using statistically averaged empirical wave models as a function of geomagnetic activity in advanced radiation belt simulations. However, statistical averages poorly characterize extreme events such as geomagnetic storms in that storm-time ultralow frequency wave power is typically larger than that derived over a solar cycle and is a poor proxy for storm-time wave power.

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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5111426PMC
http://dx.doi.org/10.1002/2016JA022618DOI Listing

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