Authors
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.
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S.‐I. Akasofu (1981) studied this question.
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