Radar observations recently made from a satellite orbiting above the ionosphere provide evidence for resonances of a plasma in a magnetic field which may be excited and detected by a dipole. The plasma may be said to be resonant, for a particular mode and frequency, if the group velocity is zero. These resonances are studied theoretically on the assumption that the dipole is of infinitesimal extent and that the plasma is excited by a charge or current impulse. The former assumption restricts the validity of the results to the asymptotic response of the plasma. The latter assumption is not a restriction. There are two electromagnetic resonances at the positive-frequency roots of ω2 ± Ωω − π2 = 0, where Ω is the electron gyro-frequency and π the electron plasma frequency, which occur at k = 0. There is also a resonance at ω = Ω, k = ∞, but this cannot be treated by the infinitesimal-dipole approximation and is deferred for separate study. ``Electrostatic'' resonances are treated in the quasi-electrostatic approximation. The resonant frequencies are π, (π2 + Ω2)½, and nΩ, n = 2, 3, …, and k = 0 at resonance. The infinitesimal-dipole model breaks down for the n = 2, 3, 4 cyclotron harmonics, but the infinitesimal line-dipole model and a line-charge model do not. The analysis shows that the oscillations decay asymptotically as an inverse power of time. The analysis also indicates that the response would be significantly stronger than is observed if measurements were made with a stationary dipole, indicating that the observed duration of the resonances is to be ascribed to the finite velocity of the satellite with respect to the exospheric plasma.
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