For each station, the latest ionogram (still image) and the ionograms for the last 24 hours (video) is displayed.
Archived data can be accessed from the links in the column to the right.
Ionograms from Kiruna
Ionograms from Lycksele
Ionograms from Uppsala
Ionograms from Lycksele (oblique from Uppsala)
Ionograms from Uppsala (oblique from Lycksele)
Responsible scientist: Thomas Leyser, thomas.leyser*irfu.se
The Swedish Institute of Space Physics operates ionosondes in Kiruna, Lycksele and Uppsala.
The frequency of the vertically transmitted wave determines the plasma density from which the pulse is relfected in the ionosphere. The time delay between transmission and reception of the reflected pulse on the ground is a measure of the height of the ionospheric layer from which the pulse was relfected. In this way the height of a specific plasma density is obtained.
An ionosonde operates by stepping the frequency of the pulses from say 1 to 20 MHz, thereby producing a map of the bottomside ionosphere. The data from such a frequency sweep is presented as the time-of-flight (virtual height) versus the transmitted frequency (the plasma frequency which is related to the plasma density). The result is an ionogram.