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Statistical analysis of relativistic electron energies for cyclotron resonance with EMIC waves observed on CRRES
Author | Meredith, Nigel; |
Keywords | Local Loss due to VLF/ELF/EMIC Waves |
Abstract | Electromagnetic ion cyclotron (EMIC) waves which propagate at frequencies below the proton gyrofrequency can undergo cyclotron resonant interactions with relativistic electrons in the outer radiation belt and cause pitch-angle scattering and electron loss to the atmosphere. Typical storm-time wave amplitudes of 1\textendash10 nT cause strong diffusion scattering which may lead to significant relativistic electron loss at energies above the minimum energy for resonance, Emin. A statistical analysis of over 800 EMIC wave events observed on the CRRES spacecraft is performed to establish whether scattering can occur at geophysically interesting energies (<=2 MeV). While Emin is well above 2 MeV for the majority of these events, it can fall below 2 MeV in localized regions of high plasma density and/or low magnetic field (fpe/fce,eq > 10) for wave frequencies just below the hydrogen or helium ion gyrofrequencies. These lower energy scattering events, which are mainly associated with resonant L-mode waves, are found within the magnetic local time range 1300 < MLT < 1800 for L > 4.5. The average wave spectral intensity of these events (4\textendash5 nT2/Hz) is sufficient to cause strong diffusion scattering. The spatial confinement of these events, together with the limited set of these waves that resonate with <=2 MeV electrons, suggest that these electrons are only subject to strong scattering over a small fraction of their drift orbit. Consequently, drift-averaged scattering lifetimes are expected to lie in the range of several hours to a day. EMIC wave scattering should therefore significantly affect relativistic electron dynamics during a storm. The waves that resonate with the \~MeV electrons are produced by low-energy (\~keV) ring current protons, which are expected to be injected into the inner magnetosphere during enhanced convection events. |
Year of Publication | 2003 |
Journal | Journal of Geophysical Research |
Volume | 108 |
Number of Pages | |
Section | |
Date Published | 06/2003 |
ISBN | |
URL | http://onlinelibrary.wiley.com/doi/10.1029/2002JA009700/full |
DOI | 10.1029/2002JA009700 |