Articles | Volume 32, issue 10
https://doi.org/10.5194/angeo-32-1349-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/angeo-32-1349-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Thin current sheets with strong bell-shape guide field: Cluster observations and models with beams
I. Y. Vasko
Space Research Institute of Russian Academy of Sciences, Moscow, Russia
A. V. Artemyev
Space Research Institute of Russian Academy of Sciences, Moscow, Russia
A. A. Petrukovich
Space Research Institute of Russian Academy of Sciences, Moscow, Russia
H. V. Malova
Space Research Institute of Russian Academy of Sciences, Moscow, Russia
Related authors
A. V. Artemyev, I. Y. Vasko, V. N. Lutsenko, and A. A. Petrukovich
Ann. Geophys., 32, 1233–1246, https://doi.org/10.5194/angeo-32-1233-2014, https://doi.org/10.5194/angeo-32-1233-2014, 2014
I. Y. Vasko, A. V. Artemyev, A. A. Petrukovich, R. Nakamura, and L. M. Zelenyi
Ann. Geophys., 32, 133–146, https://doi.org/10.5194/angeo-32-133-2014, https://doi.org/10.5194/angeo-32-133-2014, 2014
Alexander Lukin, Anton Artemyev, Evgeny Panov, Rumi Nakamura, Anatoly Petrukovich, Robert Ergun, Barbara Giles, Yuri Khotyaintsev, Per Arne Lindqvist, Christopher Russell, and Robert Strangeway
Ann. Geophys. Discuss., https://doi.org/10.5194/angeo-2020-76, https://doi.org/10.5194/angeo-2020-76, 2020
Revised manuscript not accepted
Short summary
Short summary
We have collected statistics of 81 fast plasma flow events in the magnetotail with clear MMS observations of kinetic Alfven waves (KAWs). We show that KAWs electric field magnitudes correlates with thermal/subthermal electron flux anisotropy: wider energy range of electron anisotropic population corresponds to higher KAWs’ electric field intensity. These results indicate on an important role of KAWs in production of thermal field-aligned electron population of the Earth’s magnetotail.
Marina A. Evdokimova and Anatoli A. Petrukovich
Ann. Geophys., 38, 109–121, https://doi.org/10.5194/angeo-38-109-2020, https://doi.org/10.5194/angeo-38-109-2020, 2020
Anatoli A. Petrukovich, Olga M. Chugunova, and Pavel I. Shustov
Ann. Geophys., 37, 877–889, https://doi.org/10.5194/angeo-37-877-2019, https://doi.org/10.5194/angeo-37-877-2019, 2019
Short summary
Short summary
Earth's bow shock in solar wind with high thermal and low magnetic pressure is a rare phenomenon. However, such an object is ubiquitous in astrophysical plasmas.
We surveyed statistics of such shock observations since 1995. About 100 crossings were initially identified. In this report 22 crossings from the Cluster project were studied using multipoint analysis, which allowed for the determination of the spatial scales of the shock transition and of the dominant magnetic variations
Anatoli A. Petrukovich, Olga M. Chugunova, and Pavel I. Shustov
Ann. Geophys. Discuss., https://doi.org/10.5194/angeo-2018-110, https://doi.org/10.5194/angeo-2018-110, 2018
Manuscript not accepted for further review
Short summary
Short summary
Earth's bow shock in high beta (beta is ratio of thermal
to magnetic pressure) solar wind environment is rare phenomenon.
We survey statistics of beta > 10 shock observations.
Typical solar wind parameters related with high beta are: low speed, high density and very low IMF 1–2 nT.
In this report 22 crossings are studied with spacecraft
separation within 30–200 km. Dominating magnetic waves have frequency 0.1–0.5 Hz Polarization has no stable phase
and is closer to linear.
Dominique C. Delcourt, Helmi V. Malova, and Lev M. Zelenyi
Ann. Geophys., 35, 11–23, https://doi.org/10.5194/angeo-35-11-2017, https://doi.org/10.5194/angeo-35-11-2017, 2017
Short summary
Short summary
In a magnetic field reversal, the guiding center may not be valid due to large variation of the magnetic field on the length scale of the particle gyro-radius. Although they do not execute regular helical motion and temporarily meander inside the field reversal, quasi-adiabatic particles exit this reversal with a magnetic moment nearly identical to that at entry. We show that this behavior, which is a steady-state concept, can persist during dipolarization despite the induced electric field.
Filomena Catapano, Gaetano Zimbardo, Silvia Perri, Antonella Greco, and Anton V. Artemyev
Ann. Geophys., 34, 917–926, https://doi.org/10.5194/angeo-34-917-2016, https://doi.org/10.5194/angeo-34-917-2016, 2016
Short summary
Short summary
Spacecraft observations show that energetic ions are found in the Earth’s magnetotail, with energies ranging from tens of keV to a few hundreds of keV. In this paper we carry out test particle simulations in which protons and other ion species are injected in the Vlasov magnetic field configurations obtained by Catapano et al. (2015). Three-dimensional time-dependent stochastic electromagnetic perturbations are included in the simulation box, so that the ion acceleration process is studied.
Egor V. Yushkov, Anton V. Artemyev, Anatoly A. Petrukovich, and Rumi Nakamura
Ann. Geophys., 34, 739–750, https://doi.org/10.5194/angeo-34-739-2016, https://doi.org/10.5194/angeo-34-739-2016, 2016
Short summary
Short summary
In the paper we study flapping wave structures, generated in the neutral plane of the Earth magnetotail. Investigated flapping is an important process of magnetosphere dynamics, connected with magnetic energy transformation and magnetic storm formation. Large separation of Cluster spacecraft allows us to estimate both local and global properties of flapping current sheets, the typical flapping times and propagation directions.
H. Breuillard, O. Agapitov, A. Artemyev, E. A. Kronberg, S. E. Haaland, P. W. Daly, V. V. Krasnoselskikh, D. Boscher, S. Bourdarie, Y. Zaliznyak, and G. Rolland
Ann. Geophys., 33, 583–597, https://doi.org/10.5194/angeo-33-583-2015, https://doi.org/10.5194/angeo-33-583-2015, 2015
A. V. Artemyev, I. Y. Vasko, V. N. Lutsenko, and A. A. Petrukovich
Ann. Geophys., 32, 1233–1246, https://doi.org/10.5194/angeo-32-1233-2014, https://doi.org/10.5194/angeo-32-1233-2014, 2014
I. Y. Vasko, A. V. Artemyev, A. A. Petrukovich, R. Nakamura, and L. M. Zelenyi
Ann. Geophys., 32, 133–146, https://doi.org/10.5194/angeo-32-133-2014, https://doi.org/10.5194/angeo-32-133-2014, 2014
A. V. Artemyev, A. A. Petrukovich, R. Nakamura, and L. M. Zelenyi
Ann. Geophys., 31, 1109–1114, https://doi.org/10.5194/angeo-31-1109-2013, https://doi.org/10.5194/angeo-31-1109-2013, 2013