Are high-intensity long-duration continuous AE activity (HILDCAA) events substorm expansion events?

@inproceedings{Tsurutani2004AreHL,
  title={Are high-intensity long-duration continuous AE activity (HILDCAA) events substorm expansion events?},
  author={Bruce T. Tsurutani and W Dom{\'i}nguez Gonz{\'a}lez and Fernando L. Guarnieri and Yosuke Kamide and Xiao-xiao Zhou and Jorgina Arballo},
  year={2004}
}
High-intensity, long-duration, continuous AE activity (HILDCAA) are magnetospheric/ionospheric events that occur during high-speed solar wind streams. The AE increases are caused by intermittent magnetic reconnection between southward components of interplanetary Alfven waveuctuations and magnetopause magneticelds. During solar minimum, corotating interaction regions (CIRs) created by corotating stream interactions with slow-speed streams cause relatively short duration moderate to minor… CONTINUE READING
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