Ionosphere

The ionosphere is the part of the atmosphere that contains ionized gaz, called plasma, and that affects radio propagation. It corresponds to altitudes from 50 to 500 miles at which the atmosphere is so thin that free electrons can exist.

The ionization process originates from UV solar radiation and X-Ray wavelengths. These photons are energetic enough to dislodge electrons from gaz atoms.
Simulatenously, those free electrons can be captured by positive ions. This is called recombination.
The ratio between ionization and recombination determines on overall electron density. It depends on gaz density (at lower altitudes, the recombination process accelerates) and on the amount of radiation received from space (Sun mainly, but also GRBs).

Thus, the ionosphere exhibits is a diurnal effect (day/night), a seasonal effect (summer/winter) and strong relationship with solar activity (11-years sunspot level and solar flares).

Ionosphere

The ionosphere has been divided into layers:
The Sudden Ionospheric Distubances (SIDs) and their detection
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