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Tuesday, September 27, 2011

The Origin of Ultrafast Substorm Auroras



This animation depicts the sequence of events that give rise to ultrafast substorm auroras.

A magnetic reconnection event occurs far out in the magnetotail, at a distance of around 125,000 - 200,000 km.

Energy from this event is transported by kinetic Alfvén waves (KAW) - which carry electrons - towards Earth at speeds of several thousand kilometers per second.

These KAW can reach Earth quickly enough, and carry sufficient energy, to produce intense auroras.

In reality, the reconnection process is persistent and less bursty, continuously emitting energy via the KAWs to the aurora.

Video credit: ESA/AOES Medialab

Note: For more information, see Ultrafast Substorm Auroras Explained.

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