Ionospheric storm effects in the nighttime E region caused by neutralized ring current particles
Résumé
During magnetic storms an anomalous increase in the ionization density of the nighttime E region is observed at low and middle latitudes. It has been suggested that this effect is caused by the precipitation of neutralized ring current particles. Here a coupled ring current decay-ionosphere model is used to confirm the validity of this explanation.
Origine : Accord explicite pour ce dépôt
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