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- W2009771230 abstract "We report four different types of plasma waves detected in and near the dayside polar cap boundary layer (PCBL) region at high altitudes (>6 RE). One wave type is narrowband whistler-mode emission at frequencies just below fce (5.5 kHz). These emissions could be locally generated by resonant wave-particle interactions involving an electron beam of ∼100 eV energy. A second type is a low frequency (200–300 Hz) whistler mode wave, which may be locally generated by ∼25 keV electrons or ∼45 keV ions. It is also possible that these latter waves are generated at low altitudes near the ionosphere and then converted from the ion cyclotron mode into whistler-mode during propagation from the generation region to the spacecraft. Two further types of waves are large-amplitude bipolar and monopolar solitary “electrostatic” waves. The bipolar wave structures are possibly generated all along the magnetic field lines in the field-aligned current regions (at all local times). The monopolar structures could be evolved bipolar solitary waves. A one-d schematic is presented to explain the paired monopolar structures as a result of splitting of an electron hole into two parts." @default.
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- W2009771230 date "1998-11-15" @default.
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- W2009771230 title "Plasma waves in the dayside polar cap boundary layer: Bipolar and monopolar electric pulses and whistler mode waves" @default.
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- W2009771230 doi "https://doi.org/10.1029/1998gl900114" @default.
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