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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 14, issue 11
Ann. Geophys., 14, 1134–1150, 1996
https://doi.org/10.1007/s00585-996-1134-z
© European Geosciences Union 1996
Ann. Geophys., 14, 1134–1150, 1996
https://doi.org/10.1007/s00585-996-1134-z
© European Geosciences Union 1996

  30 Nov 1996

30 Nov 1996

Low-frequency waves in the Earth's magnetosheath: present status

S. J. Schwartz, D. Burgess, and J. J. Moses S. J. Schwartz et al.
  • Astronomy Unit, Queen Mary and Westfield College, Mile End Road, London E1 4NS, United Kingdom

Abstract. The terrestrial magnetosheath contains a rich variety of low-frequency (≲ proton gyrofrequency) fluctuations. Kinetic and fluid-like processes at the bow shock, within the magnetosheath plasma, and at the magnetopause all provide sources of wave energy. The dominance of kinetic features such as temperature anisotropies, coupled with the high-β conditions, complicates the wave dispersion and variety of instabilities to the point where mode identification is difficult. We review here the observed fluctuations and attempts to identify the dominant modes, along with the identification tools. Alfvén/ion-cyclotron and mirror modes are generated by T^/T>1 temperature anisotropies and dominate when the plasma β is low or high, respectively. Slow modes may also be present within a transition layer close to the subsolar magnetopause, although they are expected to suffer strong damping. All mode identifications are based on linearized theory in a homogeneous plasma and there are clear indications, in both the data and in numerical simulations, that nonlinearity and/or inhomogeneity modify even the most basic aspects of some modes. Additionally, the determination of the wave vector remains an outstanding observational issue which, perhaps, the Cluster mission will overcome.

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