Analysis reveals shifts in the polar wall of the ionospheric trough, indicating high electron precipitation in low geomagnetic activity.
The paper analyzes experimental data on the position of the polar wall of the main ionospheric trough under low geomagnetic activity at Kr=0–1 from measurements made at the Yakutsk chain of vertical and oblique sounding ionosondes. The northern boundary of the trough under these conditions shifts to high magnetic latitudes 67–70°. This corresponds to the position of the geophysical structure “contracted oval” or compressed oval. Critical frequencies at the polar wall of the trough have high values of about 6–8 MHz. At this time, the DMSP satellite records intense 200–300 eV electron precipitation that can create the observed ionization in the F-region of the ionosphere.
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Степанов et al. (2025) studied this question.
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