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What cause partial ring current during geomagnetic storm event? 


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The partial ring current during a geomagnetic storm event is caused by a sustained enhancement of the convection electric field . This enhanced convection electric field moves plasma Earth-ward, energizing it. When the convection electric field is reduced, the particles become trapped and a symmetric ring current is formed . Substorms, which are accompanied by the injection of energetic particles, also contribute to the storm-time ring current, although the extent of their contribution is still a matter of debate . The partial ring current is predominantly located in the dusk sector, peaking in the evening magnetic local time . It forms in the early main phase of the storm, increases gradually until the storm reaches its minimum intensity, and then quickly decreases during the recovery phase . The contribution of the partial ring current weakens as the storm intensity increases .

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During some storms with positive or barely negative IMF, the model holds the ring current energy steady instead of allowing it to decrease through normal loss processes.
Open accessJournal ArticleDOI
A. T. Y. Lui, R. W. McEntire, K. B. Baker 
31 Citations
Both substorms and enhanced convection contribute to the buildup of the storm-time ring current during a geomagnetic storm event.
The partial ring current during geomagnetic storm events is primarily caused by the asymmetry of H depression and forms in the dusk sector.
The partial ring current during a geomagnetic storm event is primarily caused by a sustained enhancement of the convection electric field.
The study found that the substorm process contributes a significant amount of energy to the ring current, which may cause partial ring current during geomagnetic storm events.

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