期刊文献+

Statistical survey on the magnetic field in magnetotail current sheets: Cluster observations 被引量:3

Statistical survey on the magnetic field in magnetotail current sheets: Cluster observations
在线阅读 下载PDF
导出
摘要 The distribution properties of the magnetic field in magnetotail current sheets have been explored statistically with the magnetic measurement data of the Cluster mission from June to November of the years 2001–2005.It is found that,on average,the strength of the magnetic field and its Bz component in the current sheet are weaker in the region close to midnight but stronger near the dawnside and duskside flanks,which implies that,in general,a thinner current sheet occurs near midnight and thicker ones near both flanks.The occurrence of tail current sheet flapping is higher on both flanks than in the midnight region,although it is most frequent in the dawn flank.Current sheets with a negative Bz component or a strong By component have a higher probability of occurring at magnetic local times of 21:00–01:00,indicating that magnetic activity,e.g.magnetic reconnection and current disruption occur more frequently there.Statistically,the probability distributions of the By component and the tilt angle of magnetic field lines in the current sheet are approximately normal distributions,and the occurrence probability of the flattened current sheet is about one third that of the normal current sheet.The magnetic field and Bz component in the current sheet mainly vary from 1 nT to 10 nT.The By component in the tail central current sheet is on average twice the IMF By at 1 AU. The distribution properties of the magnetic field in magnetotail current sheets have been explored statistically with the magnetic measurement data of the Cluster mission from June to November of the years 2001 2005. It is found that, on average, the strength of the magnetic field and its Bz component in the current sheet are weaker in the region close to midnight but stronger near the dawnside and duskside flanks, which implies that, in general, a thinner current sheet occurs near midnight and thicker ones near both flanks. The occurrence of tail current sheet flapping is higher on both flanks than in the midnight region, although it is most frequent in the dawn flank. Current sheets with a negative Bz component or a strong By component have a higher probability of occurring at magnetic local times of 21:00M)1:00, indicating that magnetic activity, e.g. magnetic reconnection and current disruption occur more frequently there. Statistically, the probability distributions of the By component and the tilt angle of magnetic field lines in the current sheet are approximately normal distributions, and the occurrence probability of the flattened current sheet is about one third that of the normal current sheet. The magnetic field and Bz component in the current sheet mainly vary from 1 nT to 10 nT. The By component in the tail central current sheet is on average twice the IMF By at 1 AU.
出处 《Chinese Science Bulletin》 SCIE EI CAS 2010年第23期2542-2547,共6页
基金 supported by the National Natural Science Foundation of China (40621003 and 40674094) the National Basic Research Program of China (2006CB806305) the Hundred Talents Program of the Chinese Academy of Sciences,and the Specialized Research Fund for State Key Laboratories
关键词 统计调查 磁场分布 电流片 集群 磁尾 国际货币基金组织 概率分布 倾斜角度 magnetosphere, magnetic field, magnetotail current sheet, neutral sheet, dawn-dusk asymmetry
  • 相关文献

参考文献31

  • 1Ness N F. The Earth's magnetic tail. J Geophys Res, 1965, 70: 2989 3005.
  • 2Baumjohann W, Paschmann G, Cattell C A. Average plasma properties in the central plasma sheet. J Geophys Res, 1989, 94:6597-6606.
  • 3Baker D N, Klimas A J, Vassiliadis D, et al. Re-examination of driven and unloading aspects of magnetospheric substorms. J Geophys Res, 1997, 102:7169 7177.
  • 4Fairfield D H. A statistical determination of the shape and the position of the geomagnetic neutral sheet. J Geophys Res, 1980, 85: 775-780.
  • 5Tsyganenko N A, Fairfield D H. Global shape of the magnetotail current sheet as derived from Geotail and Polar data. J Geophys Res, 2004, 109:A03218.
  • 6Huang C Y, Frank L A. A Statistical Survey of the Central Plasma Sheet. J Geophys Res, 1994, 99:83-95.
  • 7Fairfield D H. On the average configuration of the geomagnetic tail. J Geophys Res, 1979, 84:1950-1958.
  • 8Sibeck D G, Siscoe G L, Slavin J A, et al. The distant magnetotail's response to a strong interplanetary magnetic field By-Twisting, flattening, and field line bending. J Geophys Res, 1985, 90:4011~4019.
  • 9Kaymaz Z, Siscoe G L, Luhmann J G, et al. Interplanetary magnetic field control of magnetotail magnetic field geometry: IMP 8 observations. J Geophys Res, 1994, 99:11113-11126.
  • 10Escoubet C P, Fehringer M, Goldstein M. The Cluster mission. Ann Geophys, 2001, 19:1197-1200.

同被引文献3

引证文献3

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部