Linkages Between the Radiation Belts, Polar Atmosphere and Climate: Electron Precipitation Through Wave Particle Interactions

Author(s):  
M. A. Clilverd ◽  
C. J. Rodger ◽  
M. E. Andersson ◽  
A. Seppälä ◽  
P. T. Verronen
2019 ◽  
Vol 10 (1) ◽  
Author(s):  
Mitsunori Ozaki ◽  
Yoshizumi Miyoshi ◽  
Kazuo Shiokawa ◽  
Keisuke Hosokawa ◽  
Shin-ichiro Oyama ◽  
...  

Eos ◽  
2019 ◽  
Vol 100 ◽  
Author(s):  
Richard Horne ◽  
Bruce Tsurutani

A pioneering space plasma physicist who led the way in understanding how complex wave-particle interactions control Earth’s radiation belts and low-level auroral light emissions.


1989 ◽  
Vol 94 (A11) ◽  
pp. 15243 ◽  
Author(s):  
Elena Villalón ◽  
William J. Burke ◽  
Paul L. Rothwell ◽  
Michael B. Silevitch

2015 ◽  
Vol 5 (2) ◽  
pp. 68-74 ◽  
Author(s):  
O. Agapitov ◽  
◽  
F. Mozer ◽  
A. Artemyev ◽  
D. Mourenas ◽  
...  

2014 ◽  
Vol 32 (8) ◽  
pp. 1059-1071 ◽  
Author(s):  
A. Sicard-Piet ◽  
D. Boscher ◽  
R. B. Horne ◽  
N. P. Meredith ◽  
V. Maget

Abstract. Wave particle interactions play an important role in controlling the dynamics of the radiation belts. The purpose of this study is to estimate how variations in the plasma density can affect diffusion rates resulting from interactions between chorus waves and plasmaspheric hiss with energetic particles and the resulting evolution of the energetic electron population. We perform a statistical analysis of the electron density derived from the plasma wave experiment on the CRRES satellite for two magnetic local time sectors corresponding to near midnight and near noon. We present the cumulative probability distribution of the electron plasma density for three levels of magnetic activity as measured by Kp. The largest densities are seen near L* = 2.5 while the smallest occur near L* = 6. The broadest distribution, corresponding to the greatest variability, occurs near L* = 4. We calculate diffusion coefficients for plasmaspheric hiss and whistler mode chorus for extreme values of the electron density and estimate the effects on the radiation belts using the Salammbô model. At L* = 4 and L* = 6, in the low density case, using the density from the 5th percentile of the cumulative distribution function, electron energy diffusion by chorus waves is strongest at 2 MeV and increases the flux by up to 3 orders of magnitude over a period of 24 h. In contrast, in the high density case, using the density from the 95th percentile, there is little acceleration at energies above 800 keV at L* = 6, and virtually no acceleration at L* = 4. In this case the strongest energy diffusion occurs at lower energies around 400 keV where the flux at L* = 6 increases 3 orders of magnitude.


2021 ◽  
Author(s):  
Yikai Hsieh ◽  
Yoshiharu Omura

<p>Whistler mode chorus emissions in the Earth’s magnetosphere cause energetic electron precipitation and the associated pulsating aurora. First-order cyclotron resonance in parallel whistler mode wave-particle interactions is the main mechanism of the precipitation. Not only cyclotron resonance but also Landau resonance and higher-order cyclotron resonances occur in the oblique whistler mode wave-particle interactions. Especially, electrons can be accelerated and scattered to lower equatorial pitch angles rapidly via Landau resonance. We apply test particle simulation and the Green’s function method to check the energetic electron precipitation caused by oblique chorus emissions. We simulate the wave-particle interactions around L=4.5 for electron ranges from 10 keV to a few MeV. We further compare the precipitation fluxes between parallel and oblique chorus emissions. Our simulation result reveals that oblique chorus emissions lead to more electron precipitation than parallel chorus emissions. At kinetic energy E < 100 keV, the electron precipitation ratio (oblique case/parallel case) is about 1.3. At 100 keV < E < 0.5 MeV, the ratio is greater than 2. At E > 0.5 MeV, the ratio is greater than 2 orders. Multiple resonances effect in the oblique whistler mode wave-particle interactions is the reason for the greater precipitation.</p>


Author(s):  
C. E. J. Watt ◽  
H. J. Allison ◽  
R. L. Thompson ◽  
S. N. Bentley ◽  
N. P. Meredith ◽  
...  

1998 ◽  
Vol 16 (3) ◽  
pp. 322-330 ◽  
Author(s):  
D. L. Pasmanik ◽  
V. Y. Trakhtengerts ◽  
A. G. Demekhov ◽  
A. A. Lyubchich ◽  
E. E. Titova ◽  
...  

Abstract. The formation of a zone of energetic electron precipitation by the plasmapause, a region of enhanced plasma density, following energetic particle injection during a magnetic storm, is analyzed. Such a region can also be formed by detached cold plasma clouds appearing in the outer magnetosphere by restructuring of the plasmasphere during a magnetic storm. As a mechanism of precipitation, wave-particle interactions by the cyclotron instability between whistler-mode waves and electrons are considered. In the framework of the self-consistent equations of quasi-linear plasma theory, the distribution function of trapped electrons and the electron precipitation pattern are found. The theoretical results are compared with experimental data obtained from NOAA satellites.Key words. Magnetospheric physics · Energetic particles · Precipitating and trapped · Plasma waves and instabilities


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