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Electron acceleration in the Van Allen radiation belts by fast magnetosonic waves
Author(s) -
Horne Richard B.,
Thorne Richard M.,
Glauert Sarah A.,
Meredith Nigel P.,
Pokhotelov Dimitry,
Santolík Ondřej
Publication year - 2007
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2007gl030267
Subject(s) - van allen radiation belt , physics , van allen probes , pitch angle , electron , acceleration , computational physics , hiss , magnetosphere , whistler , proton , diffusion , electromagnetic radiation , atomic physics , magnetic field , geophysics , nuclear physics , optics , classical mechanics , quantum mechanics , thermodynamics
Local acceleration is required to explain electron flux increases in the outer Van Allen radiation belt during magnetic storms. Here we show that fast magnetosonic waves, detected by Cluster 3, can accelerate electrons between ∼10 keV and a few MeV inside the outer radiation belt. Acceleration occurs via electron Landau resonance, and not Doppler shifted cyclotron resonance, due to wave propagation almost perpendicular to the ambient magnetic field. Using quasi‐linear theory, pitch angle and energy diffusion rates are comparable to those for whistler mode chorus, suggesting that these waves are very important for local electron acceleration. Since pitch angle diffusion does not extend into the loss cone, these waves, on their own, are not important for loss to the atmosphere. We suggest that magnetosonic waves, which are generated by unstable proton ring distributions, are an important energy transfer process from the ring current to the Van Allen radiation belts.

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