Contact Disclaimer
Annales Geophysicae
Copernicus.org Home EGU Copernicus Publications Copernicus Meetings
  Home  
  General Information  
  Submission  
  Special Issues  
  Evaluation  
  Production  
  Subscription  
  Online Library  
  Recent Papers  
  Volumes and Issues  
  Special Issues  
  Topical Library  
  Library Search  
  Title and Author Search  
  Volumes and Issues      Contents of Issue 3      Special Issue     
Ann. Geophys., 20, 329-340, 2002
www.ann-geophys.net/20/329/2002/
© European Geosciences Union 2002


Statistical study of transient plasma structures in magnetotail lobes and plasma sheet boundary layer: Interball-1 observations

E. E. Grigorenko1,2, A. Fedorov3,*, and L. M. Zelenyi2
1Skobeltzyn Institute of Nuclear Physics of Moscow State University, Vorobjevy Gory, 117234, Moscow, Russia
2Space Research Institute, 84/32, Profsojuznaja, 117810, Moscow, Russia
3CESR - CNRS, 9, av. de Colonel-Roche, 31400, Toulouse, France
*on leave from Space Research Institute, Moscow
Correspondence to: E. E. Grigorenkoe, 31; (grig@afed.iki.rssi.ru)

Abstract. The present paper is devoted to the statistical study of plasma structures observed at the interface between magnetospheric lobes and the plasma sheet at distances of 15–25 RE . The majority of the registered structures are bursty earthward ion streams with energies about 10–30 keV known as "beamlets". The paper describes the results of beamlet statistical analysis for different interplanetary magnetic fields (IMF), clock-angles and various magnetospheric conditions. It is shown that the energy of beamlets increases monotonously with a distance from the neutral sheet (NS) during slightly southward IMF and quiet magnetospheric conditions. Under these conditions, beamlets are observed up to 5–6 RE over the NS. In contrast, the beamlet energy decreases with increasing distance from the NS if the IMF is northward, and the region of beamlet observation becomes much wider up to 12 RE above the NS. The same (inverse) beamlet energy dependence on the distance from the NS is also registered during active magnetospheric periods. Yet, the plasma structures of various duration with quasi-isotropic ion velocity distributions resembling the plasma of the plasma sheet (PS) were observed in the same region. Statistical study performed for various IMF clock-angles demonstrates the clear difference in the spatial distributions of such plasma structures for two extreme IMF directions. When IMF is primarily northward, PS-like plasma fills the lobe region almost entirely and could be associated with the PS expansions. For primarily southward IMF time intervals, the probability of observing PS-like structures of long duration sharply decreases with the increasing distance from the NS, but PS-like structures of short durations (< 500 s) are distributed almost uniformly up to 12 RE above the NS. This feature cannot be described in terms of the PS flapping motions and requires another explanation. Relevance and limitations of the existing models attempting to explain the generation mechanisms of these transient structures are briefly discussed in the concluding part of the paper.

Key words. Magnetospheric physics (magnetotail; magnetotail boundary layers; plasma sheet)


Full Article in PDF (485 KB)
  Library Search ANGEO  
       
  Special Services  
  Printer-friendly Version  
  Bookmark  
  Download Acrobat Reader  
  News  
  ISI Impact Factor: 1.427 (2007)
 
Annales Geophysicae is launching a new section: AnGeo Communicates
 
© Copernicus 2004–2006