Plasma sheet oscillations and their relation to substorm development: Cluster and double star TC1 case study |
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Authors: | T. Takada,R. Nakamura,Y. Asano,W. Baumjohann,A. Runov,M. Volwerk,T.L. Zhang,Z. Vö rö s,K. Keika,B. Klecker,H. Rè me,E.A. Lucek,C. Carr,H.U. Frey |
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Affiliation: | 1. Space Research Institute, Austrian Academy of Sciences, Schmiedlst. 6, A-8042 Graz, Austria;2. Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency, Yoshinodai 3-1-1, Sagamihara 229-8510, Japan;3. Tokyo Institute of Technology, Ookayama 2-12-1, Meguro, Tokyo 152-8550, Japan;4. Max-Planck-Institut für extraterrestrische Physik, Postfach 1312, D-8574 Garching, Germany;5. Institute of Atmospheric Physics, AS CR, 14131 Bo?n?´ II 1401, Prague 4, Czech Republic;6. CESR/CNRS, 9 Avenue du Colonel Roche, F-31028 Toulouse Cedex 4, France;g Imperial College, Prince Consort Road, London SW7 2BZ, UK;h Space Sciences Laboratory, University of California, 7 Gauss Way #7450, Berkeley, CA 94720-7450, USA |
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Abstract: | We examined two consecutive plasma sheet oscillation and dipolarization events observed by Cluster in the magnetotail, which are associated with a pseudo-breakup and a small substorm monitored by the IMAGE spacecraft. Energy input from the solar wind and an associated enhancement of the cross-tail current lead to current sheet thinning and plasma sheet oscillations of 3–5 min periods, while the pseudo-breakups occur during the loading phase within a spatially limited area, accompanied by a localized dipolarization observed by DSP TC1 or GOES 12. That is, the so-called “growth phase” is a preferable condition for both pseudo-breakup and plasma sheet oscillations in the near-Earth magnetotail. One of the plasma sheet oscillation events occurs before the pseudo-breakup, whereas the other takes place after pseudo-breakup. Thus there is no causal relationship between the plasma sheet oscillation events and pseudo-breakup. As for the contribution to the subsequent small substorm, the onset of the small substorm took place where the preceding plasma sheet oscillations can reach the region. |
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Keywords: | Magneosphere Plasma sheet Substorm Pseudo-breakup Oscillation |
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