Behaviour of foF2 over European mid-latitudes

Computer Science

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F 2 Region, Ionospheric Disturbances, Ionospheric Electron Density, Midlatitude Atmosphere, Plasma Frequencies, Critical Frequencies, Europe

Scientific paper

Hourly monthly median values of foF2, measured at several European stations over the solar cycle were fitted to the linear regression model foF2 = aR + b, and the coefficients a and b were determined for constant cos chi values for each month in each station, to determine the sources of the seasonal and long-term diurnal variations of the foF2. The results show that the coefficient a is the most responsible factor for the winter-summer anomaly, while the coefficient b showed a diurnal anomaly. These anomalies appear to be related to corresponding variations of the the neutral-atmosphere composition at ionospheric heights.

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