Cluster observations in the magnetosheath – Part 2: Intensity of the turbulence at electron scales
The Cluster STAFF Spectral Analyser measures the magnetic and electric power spectral densities (PSD) δ<i>B</i><sup>2</sup> and δ<i>E</i><sup>2</sup> in the magnetosheath between 8 Hz and 4 kHz, i.e. between about the lower hybrid...
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Copernicus Publications
2006-12-01
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Series: | Annales Geophysicae |
Online Access: | https://www.ann-geophys.net/24/3523/2006/angeo-24-3523-2006.pdf |
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language |
English |
format |
Article |
sources |
DOAJ |
author |
C. Lacombe A. A. Samsonov A. Mangeney M. Maksimovic N. Cornilleau-Wehrlin C. C. Harvey J.-M. Bosqued P. Trávníček |
spellingShingle |
C. Lacombe A. A. Samsonov A. Mangeney M. Maksimovic N. Cornilleau-Wehrlin C. C. Harvey J.-M. Bosqued P. Trávníček Cluster observations in the magnetosheath – Part 2: Intensity of the turbulence at electron scales Annales Geophysicae |
author_facet |
C. Lacombe A. A. Samsonov A. Mangeney M. Maksimovic N. Cornilleau-Wehrlin C. C. Harvey J.-M. Bosqued P. Trávníček |
author_sort |
C. Lacombe |
title |
Cluster observations in the magnetosheath – Part 2: Intensity of the turbulence at electron scales |
title_short |
Cluster observations in the magnetosheath – Part 2: Intensity of the turbulence at electron scales |
title_full |
Cluster observations in the magnetosheath – Part 2: Intensity of the turbulence at electron scales |
title_fullStr |
Cluster observations in the magnetosheath – Part 2: Intensity of the turbulence at electron scales |
title_full_unstemmed |
Cluster observations in the magnetosheath – Part 2: Intensity of the turbulence at electron scales |
title_sort |
cluster observations in the magnetosheath – part 2: intensity of the turbulence at electron scales |
publisher |
Copernicus Publications |
series |
Annales Geophysicae |
issn |
0992-7689 1432-0576 |
publishDate |
2006-12-01 |
description |
The Cluster STAFF Spectral Analyser measures the magnetic and electric power
spectral densities (PSD) δ<i>B</i><sup>2</sup> and δ<i>E</i><sup>2</sup> in the magnetosheath
between 8 Hz and 4 kHz, i.e. between about the lower hybrid frequency
and 10 times the proton plasma frequency. We study about 23 h
of data on four different days. We do not consider the whistler waves and the
electrostatic pulses (which are not always observed)
but the underlying permanent fluctuations. Paper 1 (Mangeney et al.,
2006) shows why the permanent PSD at a given frequency <i>f</i> depends
strongly on the angle Θ<i><sub>BV</sub></i> between the magnetic field <i><b>B</b></i> and the
flow velocity <i><b>V</b></i>: this is observed for the electromagnetic (e.m.)
fluctuations, δ<i>B</i><sup>2</sup> and δ<i>E<sub>em</sub></i><sup>2</sup>, below the electron cyclotron
frequency <i>f<sub>ce</sub></i>, and for the electrostatic (e.s.) fluctuations
δ<i>E<sub>es</sub></i><sup>2</sup> at and above <i>f<sub>ce</sub></i>. This dependence is due to the Doppler
shift of fluctuations which have a highly anisotropic distribution of the
intensity of the wave vector <i><b>k</b></i> spectrum, and have a power law intensity
∝<i>k</i><sup>−ν</sup> with ν≃3 to 4. In the present paper, we look for
parameters, other
than Θ<sub><i>BV</i></sub>, which control the intensity of the fluctuations. At
<i>f</i>≃10 Hz, δ<i>B</i><sup>2</sup> and δ<i>E</i><sup>2</sup><sub><i>em</i></sub> increase when the solar
wind dynamic pressure <i>P<sub>DYN</sub><sup>SW</sup></i> increases. When <i>P<sub>DYN</sub><sup>SW</sup> </i>increases,
the magnetosheath <i>P<sub>DYN</sub><sup>MS</sup></i>∝<i>N V<sup>2</sup></i> also increases, so that
the local Doppler shift (<i><b>k.V</b></i>) increases for a given <i><b>k</b></i>. If
<i><b>V</b></i> increases, a given frequency <i>f</i> will be reached by fluctuations with a
smaller <i>k</i>, which are more intense: the variations of δ<i>B</i><sup>2</sup> (10 Hz)
with <i>P<sub>DYN</sub><sup>SW</sup></i> are only due to the Doppler shift in the spacecraft frame.
We show that the e.m. spectrum in the plasma frame has an invariant shape
<i>I<sub>1D</sub></i>∝<i>A<sub>em</sub></i> (<i>kc/ω<sub>pe</sub></i>)<sup>−ν</sup> related to the electron
inertial length <i>c/ω<sub>pe</sub></i>: the intensity <i>A<sub>em</sub></i> does not depend
on <i>P<sub>DYN</sub></i>, nor on the electron to proton temperature ratio
<i>T<sub>e</sub>/T<sub>p</sub></i>, nor on the upstream bow shock angle θ<i><sub>BN</sub></i>.
Then, we show results of 3-D MHD numerical
simulations of the magnetosheath plasma, which map the regions
where the angle Θ<sub><i>BV</i></sub> is ≃90°. The e.m. fluctuations
are more intense in these magnetosheath regions, in the spacecraft frame where
they are observed in the "whistler" range; and the e.s. fluctuations are less
intense in these same regions, in the spacecraft frame where they are observed
in the "ion acoustic" range. We conclude that the intensity of the permanent
fluctuations in the e.m. range only depends on the Doppler shift, so
that from day to day and from place to place in the magnetosheath, the
<i><b>k</b></i> spectrum in the plasma frame has an invariant shape and a constant
intensity. This is observed on scales ranging from
<i>kc/ω<sub>pe</sub></i>≃0.3 (50 km) to <i>kc/ω<sub>pe</sub></i>≃30 (500 m),
i.e. at electron scales smaller than the Cluster separation. |
url |
https://www.ann-geophys.net/24/3523/2006/angeo-24-3523-2006.pdf |
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spelling |
doaj-cbb48908c7554fa4bd5c7bfaf320c27c2020-11-24T22:55:18ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762006-12-01243523353110.5194/angeo-24-3523-2006Cluster observations in the magnetosheath – Part 2: Intensity of the turbulence at electron scalesC. Lacombe0A. A. Samsonov1A. Mangeney2M. Maksimovic3N. Cornilleau-Wehrlin4C. C. Harvey5J.-M. Bosqued6P. Trávníček7LESIA/CNRS, Observatoire de Paris, Meudon, FranceInstitute of Physics, St. Petersburg State University, St. Petersburg, RussiaLESIA/CNRS, Observatoire de Paris, Meudon, FranceLESIA/CNRS, Observatoire de Paris, Meudon, FranceCentre d'étude des Environnements Terrestre et Planétaire/UVSQ, Vélizy, FranceCentre d'Etude Spatiale des Rayonnements/CNRS, Toulouse, FranceCentre d'Etude Spatiale des Rayonnements/CNRS, Toulouse, FranceInstitute of Atmospheric Physics, Prague, Czech RepublicThe Cluster STAFF Spectral Analyser measures the magnetic and electric power spectral densities (PSD) δ<i>B</i><sup>2</sup> and δ<i>E</i><sup>2</sup> in the magnetosheath between 8 Hz and 4 kHz, i.e. between about the lower hybrid frequency and 10 times the proton plasma frequency. We study about 23 h of data on four different days. We do not consider the whistler waves and the electrostatic pulses (which are not always observed) but the underlying permanent fluctuations. Paper 1 (Mangeney et al., 2006) shows why the permanent PSD at a given frequency <i>f</i> depends strongly on the angle Θ<i><sub>BV</sub></i> between the magnetic field <i><b>B</b></i> and the flow velocity <i><b>V</b></i>: this is observed for the electromagnetic (e.m.) fluctuations, δ<i>B</i><sup>2</sup> and δ<i>E<sub>em</sub></i><sup>2</sup>, below the electron cyclotron frequency <i>f<sub>ce</sub></i>, and for the electrostatic (e.s.) fluctuations δ<i>E<sub>es</sub></i><sup>2</sup> at and above <i>f<sub>ce</sub></i>. This dependence is due to the Doppler shift of fluctuations which have a highly anisotropic distribution of the intensity of the wave vector <i><b>k</b></i> spectrum, and have a power law intensity ∝<i>k</i><sup>−ν</sup> with ν≃3 to 4. In the present paper, we look for parameters, other than Θ<sub><i>BV</i></sub>, which control the intensity of the fluctuations. At <i>f</i>≃10 Hz, δ<i>B</i><sup>2</sup> and δ<i>E</i><sup>2</sup><sub><i>em</i></sub> increase when the solar wind dynamic pressure <i>P<sub>DYN</sub><sup>SW</sup></i> increases. When <i>P<sub>DYN</sub><sup>SW</sup> </i>increases, the magnetosheath <i>P<sub>DYN</sub><sup>MS</sup></i>∝<i>N V<sup>2</sup></i> also increases, so that the local Doppler shift (<i><b>k.V</b></i>) increases for a given <i><b>k</b></i>. If <i><b>V</b></i> increases, a given frequency <i>f</i> will be reached by fluctuations with a smaller <i>k</i>, which are more intense: the variations of δ<i>B</i><sup>2</sup> (10 Hz) with <i>P<sub>DYN</sub><sup>SW</sup></i> are only due to the Doppler shift in the spacecraft frame. We show that the e.m. spectrum in the plasma frame has an invariant shape <i>I<sub>1D</sub></i>∝<i>A<sub>em</sub></i> (<i>kc/ω<sub>pe</sub></i>)<sup>−ν</sup> related to the electron inertial length <i>c/ω<sub>pe</sub></i>: the intensity <i>A<sub>em</sub></i> does not depend on <i>P<sub>DYN</sub></i>, nor on the electron to proton temperature ratio <i>T<sub>e</sub>/T<sub>p</sub></i>, nor on the upstream bow shock angle θ<i><sub>BN</sub></i>. Then, we show results of 3-D MHD numerical simulations of the magnetosheath plasma, which map the regions where the angle Θ<sub><i>BV</i></sub> is ≃90°. The e.m. fluctuations are more intense in these magnetosheath regions, in the spacecraft frame where they are observed in the "whistler" range; and the e.s. fluctuations are less intense in these same regions, in the spacecraft frame where they are observed in the "ion acoustic" range. We conclude that the intensity of the permanent fluctuations in the e.m. range only depends on the Doppler shift, so that from day to day and from place to place in the magnetosheath, the <i><b>k</b></i> spectrum in the plasma frame has an invariant shape and a constant intensity. This is observed on scales ranging from <i>kc/ω<sub>pe</sub></i>≃0.3 (50 km) to <i>kc/ω<sub>pe</sub></i>≃30 (500 m), i.e. at electron scales smaller than the Cluster separation.https://www.ann-geophys.net/24/3523/2006/angeo-24-3523-2006.pdf |