Auroral riometer absorptions and the F-region disturbances observed over a wide range of latitudes

Physics

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Auroral Zones, Equatorial Atmosphere, F Region, Magnetic Storms, Riometers, Traveling Ionospheric Disturbances, Atmospheric Attenuation, Spread F

Scientific paper

A comparison of standard riometer data from a southern auroral station with ionograms obtained at five stations positioned from sub-auroral to equatorial latitudes is presented. It is found that the rapid onset in riometer absorption, during intense substorm activities in an equinoctial period, was associated with a sequential propagation of ionospheric disturbances deduced from the F-region parameters virtual height and range spread-F. The time shift between absorption maxima and extrapolated commencement times of the disturbances was determined to be consistent with the presence of large-scale traveling ionospheric disturbances (TID), propagating equatorwards with velocities lying typically in the range 600-900 m/s, and with a median velocity of 720 m/s. These results indicate that the onset of TIDs is associated with high-energy particle precipitation, manifested by the occurrence of auroral absorption events. Results of a previous riometer study indicate that large-scale TIDs are simultaneously generated in both hemispheres.

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