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probe. In the region of the South Atlantic anomaly of the geomagnetic field, quick changes of the ion sheath capacitance have been observed indicating charging up of the probe. These quick changes are separated into two types; the first is the quick sharp variation and the second is the gradual variation. The sharp variation of the sheath capacitance value is disclosed to be triggered by the telemetry radio wave in the region of the South Atlantic anomaly.

Electron Density Distribution and Particle Precipitation in South Atlantic Anomaly: Report on Gyro-Plasma Probe Observation Installed on TAIYO