Abstract
During moderately disturbed periods, the AE and Dst indices have a simple linear relationship. However, it is shown that their relationship is considerably different during geomagnetic storms. As the |Dst| index grows above 50γ, the AE index levels off and tends to decrease. This finding may have interesting implications in understanding the formation of the ring current belt.
Full Text
Published Version
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call