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Annales Geophysicae 25, 11 (2007) 2439-2451
Internal structure and spatial dimensions of whistler wave regions in the magnetopause boundary layer
G. Stenberg 1, 2, T. Oscarsson 1, M. André 2, A. Vaivads 2, M. Backrud-Ivgren 2, 3, Y. Khotyaintsev 2, L. Rosenqvist 2, F. Sahraoui 4, N. Cornilleau-Wehrlin 4, A. Fazakerley 5, R. Lundin 6, P. M. E. Décréau 7
(29/11/2007)

We use whistler waves observed close to the magnetopause as an instrument to investigate the internal structure of the magnetopause-magnetosheath boundary layer. We find that this region is characterized by tube-like structures with dimensions less than or comparable with an ion inertial length in the direction perpendicular to the ambient magnetic field. The tubes are revealed as they constitute regions where whistler waves are generated and propagate. We believe that the region containing tube-like structures extend several Earth radii along the magnetopause in the boundary layer. Within the presumed wave generating regions we find current structures moving at the whistler wave group velocity in the same direction as the waves.
1 :  Department of Physics
Department of Physics
2 :  Swedish Institute of Space Physics
Swedish Institute of Space Physics
3 :  Division of Plasma Physics
Alfven Laboratory
4 :  Centre d'étude des environnements terrestre et planétaires (CETP)
CNRS : UMR8639 – INSU – Université de Versailles Saint-Quentin-en-Yvelines
5 :  MSSL
MSSL
6 :  Swedish Institute of Space Physics
Swedish Institute of Space Physics
7 :  Laboratoire de physique et chimie de l'environnement (LPCE)
CNRS : UMR6115 – INSU – Université d'Orléans
Planète et Univers/Océan, Atmosphère

Planète et Univers/Sciences de la Terre
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