HF modulated ionospheric currents
Joseph Allen Payne, U. S. Inan, F. R. Foust, Timothy W. Chevalier, T. F. Bell
Abstract
Joseph Allen Payne, U. S. Inan, F. R. Foust, Timothy W. Chevalier, T. F. Bell
Abstract
The HAARP HF facility is used to modulate the components of the auroral electrojet that flow in the D‐region of the ionosphere, creating ELF/VLF radiation which is then measured at a receiver co‐located with the HAARP HF antenna. An HF heating model is coupled to a full wave plasma interaction FDTD code to determine the ELF/VLF response of the ionospheric plasma to the modulated HF stimulation. The predicted FDTD fields on the ground are found to be in remarkable agreement with those measured at a receiver co‐located with HAARP. The FDTD code also predicts an upwardly propagating whistler mode that is tightly bound to the magnetic field lines.
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The HAARP HF facility is used to modulate the components of the auroral electrojet that flow in the D‐region of the ionosphere, creating ELF/VLF radiation which is then measured at a receiver co‐located with the HAARP HF antenna. An HF heating model is coupled to a full wave plasma interaction FDTD code to determine the ELF/VLF response of the ionospheric plasma to the modulated HF stimulation. The predicted FDTD fields on the ground are found to be in remarkable agreement with those measured at a receiver co‐located with HAARP. The FDTD code also predicts an upwardly propagating whistler mode that is tightly bound to the magnetic field lines.
Key concepts: Ionosphere, Electrojet, Whistler, Finite-difference time-domain method, Physics, Ionospheric heater, Antenna (radio), Geophysics