Relations of the energetic proton fluxes in the central plasma sheet with solar wind and geomagnetic activities

2013 ◽  
Vol 118 (11) ◽  
pp. 7226-7236 ◽  
Author(s):  
Jinbin Cao ◽  
Aiying Duan ◽  
Henri Reme ◽  
Iannis Dandouras
Keyword(s):  
Solar Wind ◽  
Plasma Sheet ◽  
Energetic Proton ◽  
Proton Fluxes ◽  
Central Plasma ◽  
Central Plasma Sheet ◽  
Geomagnetic Activities

scholarly journals On energetic electrons (>38 keV) in the central plasma sheet: Data analysis and modeling

2011 ◽  
Vol 116 (A9) ◽  
pp. n/a-n/a ◽  
Author(s):  
Bingxian Luo ◽  
Weichao Tu ◽  
Xinlin Li ◽  
Jiancun Gong ◽  
Siqing Liu ◽  
...  
Keyword(s):  
Data Analysis ◽  
Plasma Sheet ◽  
Energetic Electrons ◽  
Central Plasma ◽  
Central Plasma Sheet

The quasi-adiabatic ion distribution in the central plasma sheet and its boundary layer

1991 ◽  
Vol 96 (A2) ◽  
pp. 1601-1609 ◽  
Author(s):  
Maha Ashour-Abdalla ◽  
Jorg Büchner ◽  
Lev M. Zelenyi
Keyword(s):  
Boundary Layer ◽  
Plasma Sheet ◽  
Ion Distribution ◽  
Central Plasma ◽  
Central Plasma Sheet

Nonadiabatic heating of the central plasma sheet at substorm onset

1992 ◽  
Vol 97 (A2) ◽  
pp. 1481 ◽  
Author(s):  
C. Y. Huang ◽  
L. A. Frank ◽  
G. Rostoker ◽  
J. Fennell ◽  
D. G. Mitchell
Keyword(s):  
Plasma Sheet ◽  
Substorm Onset ◽  
Central Plasma ◽  
Central Plasma Sheet

Mapping of the statistical auroral distribution into the magnetosphere

1994 ◽  
Vol 72 (5-6) ◽  
pp. 266-269 ◽  
Author(s):  
Y. I. Feldstein ◽  
R. D. Elphinstone ◽  
D. J. Hearn ◽  
J. S. Murphree ◽  
L. L. Cogger
Keyword(s):  
Plasma Sheet ◽  
Large Scale ◽  
Source Region ◽  
Central Plasma ◽  
Discrete Structures ◽  
Central Plasma Sheet ◽  
Auroral Emissions ◽  
Auroral Arcs ◽  
Inner Region ◽  
Entry Layer

Statistical auroral distributions are used in combination with an empirical model of the Earth's magnetic field in an attempt to determine the large-scale magnetospheric source regions for various types of auroral luminosity. The narrow ring of structured auroral emissions during magnetically quiet intervals appears to be associated with the inner region of the nightside central plasma sheet and the dayside entry layer. Under active conditions these discrete structures expand to fill the entire central plasma sheet. The high-altitude boundary plasma sheet on the other hand is more likely to be related to diffuse auroral emissions poleward of this "oval" and to high-latitude polar auroral arcs. Under this scenario, the region of the magnetosphere bounded by the inner edge of the tail current sheet, the plasmasphere, and the dayside entry layer is the source region for the most equatorward diffuse auroral precipitation.

Proton and electron fluxes in the plasma sheet transition region and their dependence on the solar wind parameters

2020 ◽  
Author(s):  
Stepanov Nikita ◽  
Viktor Sergeev ◽  
Dmitry Sormakov ◽  
Stepan Dubyagin ◽  
Andrey Runov
Keyword(s):  
Solar Wind ◽  
Transition Region ◽  
Plasma Sheet ◽  
Time Delays ◽  
High Energy ◽  
Solar Wind Parameter ◽  
Central Plasma ◽  
High Energy Tail ◽  
Solar Wind Parameters ◽  
The Impact

<p>Proton and electron spectra in the plasma sheet usually consist of spectral core and high energy tail. These two populations are formed by different processes, driven by the various combinations of the solar wind parameters.These processes include different time delays and may act differently on protons or electrons. In this work we evaluate empirically the magnitude and the time delay of the impact of different solar wind parameter combinations on the protons and electrons with energies (30-300 keV) and reveal the mechanisms behind these impacts. To do this we build a model of the fluxes at different energy channels in the transition region (nightside central plasma sheet between 6 and 15 Re) for the THEMIS spacecraft observations in 2007-2018. We use normalized values of solar wind parameter combinations (incl. speed, density, pressure, electric field, etc) as inputs of the model, with regression coefficients indicating their impact magnitudes. We investigate different time delays up to 16 hours. The model obtained shows that protons and electrons are controlled differently by solar wind parameters: dynamic pressure is important for protons, whereas solar wind speed and VBs are important for electrons. Larger time delays are required to describe higher energy electron fluxes.</p>

scholarly journals Plasma transport in the magnetotail lobes

2009 ◽  
Vol 27 (9) ◽  
pp. 3577-3590 ◽  
Author(s):  
S. Haaland ◽  
B. Lybekk ◽  
K. Svenes ◽  
A. Pedersen ◽  
M. Förster ◽  
...  
Keyword(s):  
Solar Wind ◽  
Plasma Flow ◽  
Statistical Study ◽  
Convective Transport ◽  
Plasma Transport ◽  
Electron Drift ◽  
Substantial Fraction ◽  
Density Measurements ◽  
Central Plasma ◽  
Central Plasma Sheet

Abstract. The Earth's magnetosphere is populated by particles originating from the solar wind and the terrestrial ionosphere. A substantial fraction of the plasma from these sources are convected through the magnetotail lobes. In this paper, we present a statistical study of convective plasma transport through the Earth's magnetotail lobes for various geomagnetic conditions. The results are based on a combination of density measurements from the Electric Field and Waves Experiment (EFW) and convection velocities from the Electron Drift Instrument (EDI) on board the Cluster spacecraft. The results show that variations in the plasma flow is primarily attributed to changes in the convection velocity, whereas the plasma density remains fairly constant and shows little correlation with geomagnetic activity. During disturbed conditions there is also an increased abundance of heavier ions, which combined with enhanced convection, cause an accentuation of the mass flow. The convective transport is much slower than the field aligned transport. A substantial amount of plasma therefore escape downtail without ever reaching the central plasma sheet.

Sign in / Sign up

Export Citation Format

Share Document