中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Mode conversion between Alfven and slow waves observed in the magnetotail by THEMIS

文献类型:期刊论文

作者Du, J.; Zhang, T. L.; Nakamura, R.; Wang, C.; Baumjohann, W.; Du, A. M.; Volwerk, M.; Glassmeier, K. -H.; McFadden, J. P.
刊名GEOPHYSICAL RESEARCH LETTERS
出版日期2011
卷号38页码:L07101
ISSN号0094-8276
通讯作者Du, J (reprint author), Austrian Acad Sci, Space Res Inst, Schmiedlstr 6, A-8042 Graz, Austria.
中文摘要We present the direct spacecraft observations of wave mode conversion in the magnetotail for the first time. On February 28, 2008, the satellites P4 and P3 of THEMIS observe wave signals with a period of about 100 s in the magnetotail at about 11 R-E. At the same time, geomagnetic activity is very quiet and there are no wave signals observed by the ground-based stations. From P4 observations, Alfven and slow mode waves are identified during two successive intervals, while the coexistence and slow wave regions are observed by P3. The mode conversion between the Alfven and slow mode waves takes place while THEMIS are crossing the central current sheet. The sharp curvature of the background magnetic field should be the primary reason of this mode conversion. Citation: Du, J., T. L. Zhang, R. Nakamura, C. Wang, W. Baumjohann, A. M. Du, M. Volwerk, K.-H. Glassmeier, and J. P. McFadden (2011), Mode conversion between Alfven and slow waves observed in the magnetotail by THEMIS, Geophys. Res. Lett., 38, L07101, doi: 10.1029/2011GL046989.
英文摘要We present the direct spacecraft observations of wave mode conversion in the magnetotail for the first time. On February 28, 2008, the satellites P4 and P3 of THEMIS observe wave signals with a period of about 100 s in the magnetotail at about 11 R-E. At the same time, geomagnetic activity is very quiet and there are no wave signals observed by the ground-based stations. From P4 observations, Alfven and slow mode waves are identified during two successive intervals, while the coexistence and slow wave regions are observed by P3. The mode conversion between the Alfven and slow mode waves takes place while THEMIS are crossing the central current sheet. The sharp curvature of the background magnetic field should be the primary reason of this mode conversion. Citation: Du, J., T. L. Zhang, R. Nakamura, C. Wang, W. Baumjohann, A. M. Du, M. Volwerk, K.-H. Glassmeier, and J. P. McFadden (2011), Mode conversion between Alfven and slow waves observed in the magnetotail by THEMIS, Geophys. Res. Lett., 38, L07101, doi: 10.1029/2011GL046989.
学科主题空间物理
资助信息Specialized Research Fund for State Key Laboratories; Chinese Academy of Sciences [KJCX2-YW-T13]; National Science Foundation of China (NSFC) [41004078, 40921063]; German Ministerium fur Wirtschaft und Technologie; Deutsches Zentrum fur Luft- und Raumfahrt [50OC1001]; NASA [NAS5-02009]
收录类别SCI ; EI
语种英语
公开日期2014-12-15
源URL[http://ir.nssc.ac.cn/handle/122/3306]  
专题国家空间科学中心_空间科学部
推荐引用方式
GB/T 7714
Du, J.,Zhang, T. L.,Nakamura, R.,et al. Mode conversion between Alfven and slow waves observed in the magnetotail by THEMIS[J]. GEOPHYSICAL RESEARCH LETTERS,2011,38:L07101.
APA Du, J..,Zhang, T. L..,Nakamura, R..,Wang, C..,Baumjohann, W..,...&McFadden, J. P..(2011).Mode conversion between Alfven and slow waves observed in the magnetotail by THEMIS.GEOPHYSICAL RESEARCH LETTERS,38,L07101.
MLA Du, J.,et al."Mode conversion between Alfven and slow waves observed in the magnetotail by THEMIS".GEOPHYSICAL RESEARCH LETTERS 38(2011):L07101.

入库方式: OAI收割

来源:国家空间科学中心

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