Spectral analysis and step response of radio frequency scattering from a heated ionospheric volume

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Frequency Response, Ionospheric Heating, Radio Scattering, Spectrum Analysis, Backscattering, Data Processing, Doppler Effect, F Region, Ionospheric Propagation, Radio Frequencies, Signal To Noise Ratios, Spectral Line Width

Scientific paper

Results of a spectral analysis of field-aligned VHF backscatter from a heated ionospheric volume in the F layer are reported. The spectra fall roughly into one of three categories: narrow band (in relation to the 100-Hz unambiguous frequency interval), noiselike (essentially uniform over at least 100 Hz), and composite structure, consisting of a narrow-band peak and a noiselike wide-band component. Signal bandwidths are found to be range dependent, with the narrowest spectral widths consistently being observed at the southern periphery of the heated volume. Ionospheric drift velocities along a nominally north-south axis are found to range from 0 to 30 m/s. The result of a measurement of cross-section decay in response to step function heater power variation suggests that the Fourier component of the electron density fluctuations at half the radar wavelength smooths out by a diffusion process in planes perpendicular to B, with a time constant proportional to lambda squared. This interpretation is consistent with other observations in which the scattering is always found to decay slower at longer radar wavelengths.

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