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     
Ann. Geophys., 23, 997-1011, 2005
www.ann-geophys.net/23/997/2005/
© European Geosciences Union 2005


Correlation between ground-based observations of substorm signatures and magnetotail dynamics

E. Borälv1, H. J. Opgenoorth1,9, K. Kauristie2, M. Lester3, J.-M. Bosqued4, J. P. Dewhurst5, C. J. Owen5, M. Dunlop6,8, J. A. Slavin7, A. Fazakerley5, and C. Perry8
1Swedish Institute of Space Physics, Uppsala, Sweden
2Finnish Meteorological Institute, Space Research, Helsinki, Finland
3University of Leicester, Department of Physics and Astronomy, Leicester, UK
4Centre d’Etude Spatiale des Rayonnements, Toulouse, France
5Mullard Space Science Laboratory, University College London, Surrey, UK
6Space and Atmospheric Physics, Blackett Laboratory, Imperial College, London, UK
7NASA Goddard Space Flight Center, Laboratory for Extraterrestrial Physics, Maryland, USA
8Space Science Department, Rutherford Appleton Laboratory, Oxfordshire, UK
9European Space Agency, ESTEC, Noordwijk, Netherlands

Abstract. We present a substorm event study using the four Cluster spacecraft in combination with ground-based instruments, in order to perform simultaneous observations in the ionosphere and magnetotail. We show good correlation between substorm signatures on the ground and in the magnetotail, even though data from the northern-ground and southern-tail hemispheres are compared. During this event ground-based magnetometers show a substorm onset over Scandinavia in the pre-midnight sector. Within 1.5h the onset and three intensifications are apparent in the magnetograms. For all the substorm signatures seen on the ground, corresponding plasma sheet boundary motion is visible at Cluster, located at a downtail distance of 18.5 RE. As a result of the substorm onset and intensifications, Cluster moves in and out between the southern plasma sheet and lobe. Due to the lack of an apparent solar wind driver and the good correlation between substorm signatures on the ground, we conclude the substorm itself is the driver for these plasma sheet dynamics. We show that in the scales of Cluster inter-spacecraft distances (~0.5 RE) the inferred plasma sheet motion is often directed in both Ygsm- and Zgsm-directions, and discuss this finding in the context of previous studies of tail flapping and plasma sheet thickness variations.

Full Article in PDF (3967 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