Anomalous electron precipitation near the Earth’s auroral zone induced by the wave–particle interaction

1997 ◽  
Vol 4 (6) ◽  
pp. 2269-2275 ◽  
Author(s):  
I. F. Potapenko ◽  
A. G. Elfimov ◽  
A. S. de Assis ◽  
C. A. de Azevedo
Keyword(s):  
Particle Interaction ◽  
Auroral Zone ◽  
Electron Precipitation ◽  
Wave Particle Interaction

scholarly journals Data processing in Software-type Wave–Particle Interaction Analyzer onboard the Arase satellite

2018 ◽  
Vol 70 (1) ◽  
Author(s):  
Mitsuru Hikishima ◽  
Hirotsugu Kojima ◽  
Yuto Katoh ◽  
Yoshiya Kasahara ◽  
Satoshi Kasahara ◽  
...  
Keyword(s):  
Data Processing ◽  
Particle Interaction ◽  
Wave Particle Interaction ◽  
Type Wave

Chaotic Regime of Alfvén Eigenmode Wave-Particle Interaction

2000 ◽  
Vol 85 (15) ◽  
pp. 3177-3180 ◽  
Author(s):  
R. F. Heeter ◽  
A. F. Fasoli ◽  
S. E. Sharapov
Keyword(s):  
Particle Interaction ◽  
Chaotic Regime ◽  
Wave Particle Interaction

scholarly journals Strong localized variations of the low-altitude energetic electron fluxes in the evening sector near the plasmapause

1998 ◽  
Vol 16 (1) ◽  
pp. 25-33 ◽  
Author(s):  
E. E. Titova ◽  
T. A. Yahnina ◽  
A. G. Yahnin ◽  
B. B. Gvozdevsky ◽  
A. A. Lyubchich ◽  
...  
Keyword(s):  
Sharp Increase ◽  
Electron Flux ◽  
Particle Interaction ◽  
Energetic Electron ◽  
Recovery Phase ◽  
Electron Precipitation ◽  
Statistical Characteristics ◽  
Evening Sector ◽  
Proton Precipitation ◽  
Low Altitude

Abstract. Specific type of energetic electron precipitation accompanied by a sharp increase in trapped energetic electron flux are found in the data obtained from low-altitude NOAA satellites. These strongly localized variations of the trapped and precipitated energetic electron flux have been observed in the evening sector near the plasmapause during recovery phase of magnetic storms. Statistical characteristics of these structures as well as the results of comparison with proton precipitation are described. We demonstrate the spatial coincidence of localized electron precipitation with cold plasma gradient and whistler wave intensification measured on board the DE-1 and Aureol-3 satellites. A simultaneous localized sharp increase in both trapped and precipitating electron flux could be a result of significant pitch-angle isotropization of drifting electrons due to their interaction via cyclotron instability with the region of sharp increase in background plasma density.Key words. Ionosphere (particle precipitation; wave-particle interaction) Magnetospheric Physics (plasmasphere)

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