Radio users will be familiar with dropouts in HF and VHF radio signals, which vary with time of day and solar activity.
The basic process:
- Electrons stream continuously from the Sun; but the flux density varies with solar activity
- From a point on Earth, electron flux density also has diurnal variation (maximum when facing the sun at midday, minimum at midnight)
- Electrons impacting the upper atmosphere produces ionisation which builds during the day and dissipates overnight
- HF and some VHF radio waves are absorbed in the ionised layers
- Consequently earth-side radio flux in the HF and lower VHF bands is attenuated in proportion to electron flux
Data inputs:
- One week's radio flux data from a radio-quiet VHF band (57-62MHz)
- Electron flux data from GOES 13 satellite
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