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Modell der Ionosphäre Elektronendichte der oberen Ionosphäre rund um die Erde zu einem Zeitpunkt des Tages (0:00 Uhr Universalzeit): hohe Dichten in Rot, geringe in Blau. Die weiße Linie markiert den geomagnetischen Äquator.
CCBY 4.0 Smirnov et al. (2023) - Scientific Reports (https://doi.org/10.1038/s41598-023-28034-z)
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