X. Vallières
Centre national de la recherche scientifique
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Featured researches published by X. Vallières.
Journal of Geophysical Research | 2012
Tomas Karlsson; Nils Brenning; H. Nilsson; J-G Trotignon; X. Vallières; G. Facsko
We use Cluster multipoint density measurements, using the spacecraft potential, to identify localized density enhancements (>50%) in the magnetosheath, and estimate their three-dimensional morph ...
Journal of Geophysical Research | 2008
Sandrine Grimald; P. M. E. Décréau; P. Canu; A. Rochel; X. Vallières
[1] Nonthermal continuum (NTC) radiation is, with auroral kilometric radiation (AKR), one of the two electromagnetic emissions generated within the Earth’s magnetosphere and radiated into space. It is generally believed that NTC is emitted in the plasmapause density gradient after conversion of intense electrostatic waves, present near the magnetic equator, into electromagnetic waves. In this paper, we present a specific type of NTC event, of infrequent occurrence, displaying a finger-like pattern not yet reported: banded emissions peaking at exact multiples of a common frequency, df, which decrease inbound toward the plasmapause boundary layer (PPBL). Analysis is presented that indicates that the corresponding sources are nearby sites of the PPBL where the local electron gyrofrequency fce equals df. The sources are radiating beams of limited cone angle size. The NTC sources for this event are shown to be located at about 20 magnetic latitude. This illustrates that the PPBL is active in radiating NTC waves not only near the magnetic equator but also up to the medium-latitude range.
Archive | 2017
H. Gunell; H. Nilsson; Maria Hamrin; Anders Eriksson; Elias Odelstad; Romain Maggiolo; P. Henri; X. Vallières; Kathrin Altwegg; Chia-Yu Tzou; Martin Rubin; K.-H. Glassmeier; G. Stenberg Wieser; C. Simon Wedlund; J. De Keyser; Frederik Dhooghe; Gaël Cessateur; Andrew Gibbons
Context. On 20 January 2015 the Rosetta spacecraft was at a heliocentric distance of 2.5 AU, accompanying comet 67P/Churyumov-Gerasimenko on its journey toward the Sun. The Ion Composition Analyser ...
Astronomy and Astrophysics | 2017
H. Gunell; H. Nilsson; Maria Hamrin; Anders Eriksson; Elias Odelstad; Romain Maggiolo; P. Henri; X. Vallières; Kathrin Altwegg; Chia-Yu Tzou; Martin Rubin; K.-H. Glassmeier; G. Stenberg Wieser; C. Simon Wedlund; J. De Keyser; Frederik Dhooghe; Gaël Cessateur; Andrew Gibbons
Context. On 20 January 2015 the Rosetta spacecraft was at a heliocentric distance of 2.5 AU, accompanying comet 67P/Churyumov-Gerasimenko on its journey toward the Sun. The Ion Composition Analyser ...
The Astronomical Journal | 2016
E. Vigren; Kathrin Altwegg; Niklas J. T. Edberg; Anders Eriksson; M. Galand; P. Henri; Fredrik Johansson; Elias Odelstad; Chia-Yu Tzou; X. Vallières
During 2015 January 9–11, at a heliocentric distance of ~2.58–2.57 au, the ESA Rosetta spacecraft resided at a cometocentric distance of ~28 km from the nucleus of comet 67P/Churyumov–Gerasimenko, sweeping the terminator at northern latitudes of 43°N–58°N. Measurements by the Rosetta Orbiter Spectrometer for Ion and Neutral Analysis/Comet Pressure Sensor (ROSINA/COPS) provided neutral number densities. We have computed modeled electron number densities using the neutral number densities as input into a Field Free Chemistry Free model, assuming H2O dominance and ion-electron pair formation by photoionization only. A good agreement (typically within 25%) is found between the modeled electron number densities and those observed from measurements by the Mutual Impedance Probe (RPC/MIP) and the Langmuir Probe (RPC/LAP), both being subsystems of the Rosetta Plasma Consortium. This indicates that ions along the nucleus-spacecraft line were strongly coupled to the neutrals, moving radially outward with about the same speed. Such a statement, we propose, can be further tested by observations of H3O+/H2O+ number density ratios and associated comparisons with model results.
Journal of Geophysical Research | 2009
Sandrine Grimald; Claire Foullon; P. M. E. Décréau; G. Le Rouzic; Xavier Suraud; X. Vallières
Nonthermal continuum (NTC) radiation is believed to be emitted by the conversion of an electrostatic wave into an electromagnetic one, which takes place at the Earths magnetic equator. It is generally accepted that the frequency of the electrostatic wave at the source meets a local characteristic frequency placed in between two multiples of the electron cyclotron frequency, fce, which results in emission of a narrow band frequency element. In an event on 14 August 2003, we compare oscillations of the central frequency of distinct NTC frequency elements observed from Cluster orbiting near perigee, with simultaneous Pc5 Ultra Low Frequency (ULF) pulsations in the magnetic field observed from the same platform. The latter magnetic perturbations are interpreted as magnetohydrodynamic poloidal waves, where fundamental and second harmonic modes coexist. The NTC oscillation and the fundamental wave have similar periods, but are phase shifted by a quarter of period. From the correlation between both signals, and the proximity of the NTC source (localized via triangulation) with Cluster, we infer that the poloidal perturbations are spatially uniform between the source and the satellites. From the phase shift between signals, we conclude that the electrostatic wave which converts into NTC is mainly governed by the plasma density, affected by movements of the magnetic field lines. Furthermore, we demonstrate that the observations can be used to perform a magnetoseismology of the emitting surface. The results show a steepening of the plasmapause density profile near the satellites, which can be responsible for the generation of NTC emission.
Journal of Geophysical Research | 2018
Elias Odelstad; Anders Eriksson; F. L. Johansson; E. Vigren; P. Henri; Nicolas Gilet; K. L. Heritier; X. Vallières; Martin Rubin; Mats André
A major point of interest in cometary plasma physics has been the diamagnetic cavity, an unmagnetized region in the inner-most part of the coma. Here, we combine Langmuir and Mutual Impedance Probe measurements to investigate ion velocities and electron temperatures in the diamagnetic cavity of comet 67P, probed by the Rosetta spacecraft. We find ion velocities generally in the range 2-4 km/s, significantly above the expected neutral velocity
Astronomy and Astrophysics | 2018
H. Nilsson; Herbert Gunell; Tomas Karlsson; Nils Brenning; P. Henri; C. Goetz; Anders Eriksson; E. Behar; G. Stenberg Wieser; X. Vallières
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Astronomy and Astrophysics | 2018
K. L. Heritier; M. Galand; P. Henri; F. L. Johansson; A. Beth; Anders Eriksson; X. Vallières; Kathrin Altwegg; J. L. Burch; C. M. Carr; E. Ducrot; Rajkumar Hajra; Martin Rubin
1~km/s, showing that the ions are (partially) decoupled from the neutrals, indicating that ion-neutral drag was not responsible for balancing the outside magnetic pressure. Observations of clear wake effects on one of the Langmuir probes showed that the ion flow was close to radial and supersonic, at least w.r.t. the perpendicular temperature, inside the cavity and possibly in the surrounding region as well. We observed spacecraft potentials
Astronomy and Astrophysics | 2017
Rajkumar Hajra; P. Henri; X. Vallières; M. Galand; K. L. Heritier; Anders Eriksson; Elias Odelstad; Niklas J. T. Edberg; J. L. Burch; T. W. Broiles; R. Goldstein; K.-H. Glassmeier; I. Richter; C. Goetz; Bruce T. Tsurutani; H. Nilsson; Kathrin Altwegg; Martin Rubin
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