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The poloidal waves with large azimuthal wavenumbers (m~100) in the magnetosphere are known to be generated by drift or drift bounce resonance with energetic ring current particles, and these waves may play a role in modulating the energetic particles in the inner magnetosphere. When examining the magnetic field data collected by the NASA ST-5 satellites in the low Earth orbit, Le et al.  discovered many wave events with frequencies of 30\textendash200 mHz (in the Pc 2\textendash3 band), and they proposed that these wav ...
YEAR: 2015   DOI: 10.1002/2015JA021145