2000
DOI: 10.1007/s00585-000-1390-2
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Effects of substorms on the stormtime ring current index <i>Dst</i>

Abstract: 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 ®nd that increases in Dst are mildly related to the strength of substorm expansive phase activity during the development of the storm main phase. More surprisingl… Show more

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Cited by 15 publications
(2 citation statements)
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“…[12] This result implies that surface charging by particles injected from geomagnetic tail may be the most probable cause of the severe anomalies. It is known that increase of Kp index is partly due to the collapse of stretched magnetic field lines on the night side of the Earth which also causes the injection of energetic particles from the region of geomagnetic tail [Rostoker, 2000]. In addition, during geomagnetic storms, magnetic field stretching makes nonuniform particle distribution at the geostationary orbit [Onsager et al, 2002;Lee et al, 2006].…”
Section: Local Time Dependencementioning
confidence: 99%
“…[12] This result implies that surface charging by particles injected from geomagnetic tail may be the most probable cause of the severe anomalies. It is known that increase of Kp index is partly due to the collapse of stretched magnetic field lines on the night side of the Earth which also causes the injection of energetic particles from the region of geomagnetic tail [Rostoker, 2000]. In addition, during geomagnetic storms, magnetic field stretching makes nonuniform particle distribution at the geostationary orbit [Onsager et al, 2002;Lee et al, 2006].…”
Section: Local Time Dependencementioning
confidence: 99%
“…Therefore, ap should be sensibly more responsive to electric fields that contribute to ring current enhancement (that is, to Dst changes) inside geosynchronous orbit during strong disturbances than AE or AL, which are measured inside the auroral oval (Rostoker, 2000;Thomsen, 2004). In addition, Lockwood et al (2019a) have noticed that AE saturates at high geomagnetic activity measured by am (when am > 150, with am a mid-latitude index very similar to ap) probably because the auroral oval then expands equatorward of the stations used to measure AE.…”
Section: Physical Interpretation-insights From Entropy Analysismentioning
confidence: 99%