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Ann. Geophys., 24, 3507-3521, 2006
www.ann-geophys.net/24/3507/2006/
© European Geosciences Union 2006

Cluster observations in the magnetosheath – Part 1: Anisotropies of the wave vector distribution of the turbulence at electron scales

A. Mangeney¹, C. Lacombe¹, M. Maksimovic¹, A. A. Samsonov², N. Cornilleau-Wehrlin³, C. C. Harvey⁴, J.-M. Bosqued⁴, and P. Trávníček^5
1LESIA/CNRS, Observatoire de Paris, Meudon, France
²Institute of Physics, St. Petersburg State University, St. Petersburg, Russia
³Centre d'étude des Environnements Terrestre et Planétaire/UVSQ, Vélizy, France
⁴Centre d'Etude Spatiale des Rayonnements/CNRS, Toulouse, France
⁵Institute of Atmospheric Physics, Prague, Czech Republic

Abstract. We analyse the power spectral density δB² and δE² of the magnetic and electric fluctuations measured by Cluster 1 (Rumba) in the magnetosheath during 23 h, on four different days. The frequency range of the STAFF Spectral Analyser (f=8 Hz to 4 kHz) extends from about the lower hybrid frequency, i.e. the electromagnetic (e.m.) range, up to about 10 times the proton plasma frequency, i.e. the electrostatic (e.s.) range. In the e.m. range, we do not consider the whistler waves, which are not always observed, but rather the underlying, more permanent fluctuations. In this e.m. range, δB² (at 10 Hz) increases strongly while the local angle Θ_BV between the magnetic field B and the flow velocity V increases from 0° to 90°. This behaviour, also observed in the solar wind at lower frequencies, is due to the Doppler effect. It can be modelled if we assume that, for the scales ranging from kc/ω_pe≃0.3 to 30 (c/ω_pe is the electron inertial length), the intensity of the e.m. fluctuations for a wave number k (i) varies like k^−ν with ν>≃3, (ii) peaks for wave vectors k perpendicular to B like |sinθ_kB|^µ with µ>≃100. The shape of the observed variations of δB² with f and with Θ_BV implies that the permanent fluctuations, at these scales, statistically do not obey the dispersion relation for fast/whistler waves or for kinetic Alfvén waves: the fluctuations have a vanishing frequency in the plasma frame, i.e. their phase velocity is negligible with respect to V (Taylor hypothesis). The electrostatic waves around 1 kHz behave differently: δE² is minimum for Θ_BV>≃90°. This can be modelled, still with the Doppler effect, if we assume that, for the scales ranging from k λ_De>≃0.1 to 1 (λ_De is the Debye length), the intensity of the e.s. fluctuations (i) varies like k^−ν with ν>≃4, (ii) peaks for k parallel to B like |cosθ_kB|^µ with µ>≃100. These e.s. fluctuations may have a vanishing frequency in the plasma frame, or may be ion acoustic waves. Our observations imply that the e.m. frequencies observed in the magnetosheath result from the Doppler shift of a spatial turbulence frozen in the plasma, and that the intensity of the turbulent k spectrum is strongly anisotropic, for both e.m. and e.s. fluctuations. We conclude that the turbulence has strongly anisotropic k distributions, on scales ranging from kc/ω_pe≃0.3 (50 km) to kλ_De≃1 (30 m), i.e. at electron scales, smaller than the Cluster separation.

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Citation: Mangeney, A., Lacombe, C., Maksimovic, M., Samsonov, A. A., Cornilleau-Wehrlin, N., Harvey, C. C., Bosqued, J.-M., and Trávníček, P.: Cluster observations in the magnetosheath – Part 1: Anisotropies of the wave vector distribution of the turbulence at electron scales, Ann. Geophys., 24, 3507-3521, 2006.   Bibtex   EndNote   Reference Manager