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Cluster observations and theoretical identification of broadband waves in the auroral region
Backrud-Ivgren M., Stenberg G., André M., Morooka M., Hobara Y., Joko S., Rönnmark K., Cornilleau-Wehrlin N., Fazakerley A., Rème H.
Annales Geophysicae 23, 12 (2005) 3739-3752 - http://hal.archives-ouvertes.fr/hal-00330081
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Cluster observations and theoretical identification of broadband waves in the auroral region
M. Backrud-Ivgren 1, 2, G. Stenberg 3, M. André 1, 2, M. Morooka 1, Y. Hobara 4, S. Joko 4, K. Rönnmark 3, N. Cornilleau-Wehrlin 5, A. Fazakerley 6, H. Rème 7
1 :  Swedish Institute of Space Physics
Swedish Institute of Space Physics
Suède
2 :  Dept. of Astronomy and Space Physics
Uppsala University
Suède
3 :  Department of Physics
Department of Physics
Suède
4 :  Swedish Institute of Space Physics
Swedish Institute of Space Physics
Suède
5 :  Centre d'étude des environnements terrestre et planétaires (CETP)
http://www.cetp.ipsl.fr/
CNRS : UMR8639 – INSU – Université de Versailles Saint-Quentin-en-Yvelines
10/12 avenue de l'Europe 78140 VELIZY
France
6 :  The Mullard Space Science Laboratory
University College of London (UCL)
Royaume-Uni
7 :  Centre d'étude spatiale des rayonnements (CESR)
http://www.cesr.fr
CNRS : UMR5187 – Observatoire Midi-Pyrénées – INSU – Université Paul Sabatier [UPS] - Toulouse III
9 Av du colonel Roche - BP 4346 31028 TOULOUSE CEDEX 4
France
Broadband waves are common on auroral field lines. We use two different methods to study the polarization of the waves at 10 to 180 Hz observed by the Cluster spacecraft at altitudes of about 4 Earth radii in the nightside auroral region. Observations of electric and magnetic wave fields, together with electron and ion data, are used as input to the methods. We find that much of the wave emissions are consistent with linear waves in homogeneous plasma. Observed waves with a large electric field perpendicular to the geomagnetic field are more common (electrostatic ion cyclotron waves), while ion acoustic waves with a large parallel electric field appear in smaller regions without suprathermal (tens of eV) plasma. The regions void of suprathermal plasma are interpreted as parallel potential drops of a few hundred volts.
Anglais

Annales Geophysicae (Ann. Geophys.)
Publisher European Geosciences Union (EGU)
ISSN 0992-7689 (eISSN : 1432-0576)
internationale
23/12/2005
23
12
3739-3752

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