Naturally enhanced ion acoustic waves in the auroral ionosphere observed with the EISCAT 933-MHz radar

Physics

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Auroral Zones, Earth Ionosphere, Eiscat Radar System (Europe), Ion Acoustic Waves, Ion Temperature, F Region, Incoherent Scattering, Radar Scattering, Ultrahigh Frequencies

Scientific paper

High-resolution incoherent scatter radar spectra obtained at 933 MHz by the EISCAT European Incoherent Scatter UHF radar on February 14, 1990 are presented. The spectra show intense short-lived enhancements of the ion acoustic shoulders from 138 to 587 km altitude, both along the magnetic-field-aligned direction and at angles that are within 15 deg from that direction. These observations indicate that field-aligned thermal electron drifts are destabilizing the ion acoustic waves. They confirm and extend the report of similar echoes by Foster et al. (1988). It is suggested that field-aligned flows of soft electrons depositing their energy at horizontally poor conducting F region heights are the cause of parallel electric fields in the ionosphere.

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