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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 23, issue 3
Ann. Geophys., 23, 973-982, 2005
https://doi.org/10.5194/angeo-23-973-2005
© Author(s) 2005. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ann. Geophys., 23, 973-982, 2005
https://doi.org/10.5194/angeo-23-973-2005
© Author(s) 2005. This work is distributed under
the Creative Commons Attribution 3.0 License.

  30 Mar 2005

30 Mar 2005

Optimal reconstruction of magnetopause structures from Cluster data

H. Hasegawa1,2, B. U. Ö. Sonnerup1, B. Klecker2, G. Paschmann2, M. W. Dunlop3, and H. Rème4 H. Hasegawa et al.
  • 1Thayer School of Engineering, Dartmouth College, Hanover, New Hampshire, USA
  • 2Max-Planck-Institut für extraterrestrische Physik, Garching, Germany
  • 3Space Sciences Division, Rutherford Appleton Laboratory, Oxfordshire, UK
  • 4Centre d’Etude Spatiale des Rayonnements, Toulouse, France

Abstract. The Grad-Shafranov (GS) reconstruction technique, a single-spacecraft based data analysis method for recovering approximately two-dimensional (2-D) magnetohydrostatic plasma/field structures in space, is improved to become a multi-spacecraft technique that produces a single field map by ingesting data from all four Cluster spacecraft into the calculation. The plasma pressure, required for the technique, is measured in high time resolution by only two of the spacecraft, C1 and C3, but, with the help of spacecraft potential measurements available from all four spacecraft, the pressure can be estimated at the other spacecraft as well via a relationship, established from C1 and C3 data, between the pressure and the electron density deduced from the potentials. Consequently, four independent field maps, one for each spacecraft, can be reconstructed and then merged into a single map. The resulting map appears more accurate than the individual single-spacecraft based ones, in the sense that agreement between magnetic field variations predicted from the map to occur at each of the four spacecraft and those actually measured is significantly better. Such a composite map does not satisfy the GS equation any more, but is optimal under the constraints that the structures are 2-D and time-independent. Based on the reconstruction results, we show that, even on a scale of a few thousand km, the magnetopause surface is usually not planar, but has significant curvature, often with intriguing meso-scale structures embedded in the current layer, and that the thickness of both the current layer and the boundary layer attached to its earthward side can occasionally be larger than 3000km.

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