A modelling study of satellite beacon measurements of protonospheric replenishment

Physics

Scientific paper

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Atmospheric Models, Beacon Satellites, Plasmasphere, Proton Belts, Satellite Observation, Arctic Regions, Diurnal Variations, Hydrogen Ions, Midlatitude Atmosphere, Oxygen Ions

Scientific paper

Recent satellite beacon derived measurements of the recovery of protonospheric ionization following periods of increased geomagnetic activity show that the recovery takes longer than is indicated by whistler measurements. Realistic plasmasphere models have been used to determine whether satellite beacon measurements are reliable indicators of this recovery. It is found that the recovery time of the protonospheric content is similar to that of the minimum L-value flux tube intersected by the slant raypaths. Satellite beacon results are therefore useful indicators of protonospheric recovery after a storm provided any unrepresentative diurnal variations are eliminated.

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