Abstract

There has been some discussion in recent times regarding whether or not substorm expansive phase activity plays any role of importance in the formation of the stormtime ring current. I explore this question using the Kp index as a proxy for substorm expansive phase activity and the Dst index as a proxy for symmetric ring current strength. I find that increases in Dst are mildly related to the strength of substorm expansive phase activity during the development of the storm main phase. More surprisingly, I find that the strength of Dst during the storm recovery phase is positively correlated with the strength of substorm expansive phase activity. This result has an important bearing on the question of how much the Dst index reflects activity other than that of the stormtime symmetric ring current strength for which it is supposed to be a proxy.Key words: Ionosphere (electric fields and currents) - Magnetospheric physics (current systems; storms and substorms)

Highlights

  • RostokerEffects of substorms on the stormtime ring current index Dst. Annales Geophysicae, European Geosciences Union, 2000, 18 (11), pp.1390-1398

  • It has been known for some time that the negative Hcomponent depressions of up to several hundred nT observed at low-latitude magnetic observatories are due to large-scale currentsowing around the Earth carried by gradient/curvature drifting charged particles (Singer, 1957)

  • This research was started with the aim of trying to see if there was any clear relationship between substorm expansive phase (EP) activity and the development of the symmetric ring current

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Summary

Rostoker

Substorm e€ect on Dst substorm expansive phases are not responsible for symmetric ring current growth and, may limit that growth. There is good reason to study the response of Dst to substorm EP activity and my purpose here is to explore that question further

Introduction
Processing of the data and presentation format
Presentation of the data
Discussion of the results
Conclusions
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