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Mitigation of energetic electrons in the magnetosphere by amplified whistler wave under double cyclotron resonances

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Figure

Fig. 1. Temporal evolution of the amplitude of a whistler wavepropagating in the magnetosphere.
Fig. 2. (a) Wave amplitude verses time for four different incidentwave intensities and (b) amplitude gain G of amplified whistlerwave verses the incident wave intensity.
Fig. 3. Surface of section plot from the trajectories of four electronswith initial energies γ0=1.2 (in blue), 1.5 (in green), 2 (in orange),and 3 (in red), and with the same initial pitch angle θ0=60◦ andwave amplitude �1=0.08 in a system with �0=8 and ωb
Fig. 4.tron interacting with a whistler wave at Doppler shifted cyclotronresonance.B Temporal evolution of the pitch angle of a 1.5 MeV elec-4Plots A and B correspond to wave magnetic field=7×10− 41B0 and 8.1×10−B0 cases, respectively.
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