Drift theory of the resonant interaction of charged particles with wave packets

1982 ◽  
Vol 25 (4) ◽  
pp. 299-301 ◽  
Author(s):  
V. P. Milant'ev
2003 ◽  
Vol 48 (8) ◽  
pp. 441-446
Author(s):  
S. Yu. Annenkov ◽  
N. N. Romanova

1985 ◽  
Vol 116 (1) ◽  
pp. 107-129 ◽  
Author(s):  
R. A. Burger ◽  
H. Moraal ◽  
G. M. Webb

1982 ◽  
Vol 24 (12) ◽  
pp. 1491-1493 ◽  
Author(s):  
V P Milantiev ◽  
T Ortis

2020 ◽  
pp. 73-77
Author(s):  
V.А. Buts ◽  
V.V. Kuzmin ◽  
A.P. Tolstoluzhsky

The possibilities and conditions of effective interaction, in particular acceleration, of charged particles by the field of an intense plane electromagnetic wave in the presence of an external constant magnetic field are considered. It is shown that the well-known conditions of cyclotron resonances require generalization. New conditions for the resonant interaction of charged particles are formulated, which contain not only the strength of the external magnetic field (as the well-known conditions of cyclotron resonances) but also the field strength of the wave. Cases of both small wave field strengths, so large, are considered. It is shown that new resonance conditions open up new possibilities for effective particle acceleration.


2013 ◽  
Vol 99 ◽  
pp. 73-77 ◽  
Author(s):  
Rumen Shkevov ◽  
Nikolay Sergeevich Erokhin ◽  
Ludmila Anatolievna Mikhailovskaya ◽  
Nadezhda Nikolaevna Zolnikova

2009 ◽  
Vol 51 (A) ◽  
pp. 129-135 ◽  
Author(s):  
KEN-ICHI MARUNO ◽  
YASUHIRO OHTA ◽  
MASAYUKI OIKAWA

AbstractAn integrable two-component analogue of the two-dimensional long wave – short wave resonance interaction (2c-2d-LSRI) system is studied. Wronskian solutions of 2c-2d-LSRI system are presented. A reduced case, which describes resonant interaction between an interfacial wave and two surface wave packets in a two-layer fluid, is also discussed.


1989 ◽  
Vol 23 (6) ◽  
pp. 857-861 ◽  
Author(s):  
M. B. Zel'man ◽  
B. V. Smorodskii

2021 ◽  
Author(s):  
Veronika Grach ◽  
Andrei Demekhov ◽  
Alexey Larchenko

Abstract We study the influence of real structure of electromagnetic ion-cyclotron wave packets in the Earth’s radiation belts on precipitation of relativistic electrons. Automatic algorithm is used to distinguish isolated elements (wave packets) and obtain their amplitude and frequency profiles from satellite observations by Van Allen Probe B. We focus on rising-tone EMIC wave packets in the proton band, with a maximum amplitude of 1.2-1.6 nT. The resonant interaction of the considered wave packets with relativistic electrons 1.5-9 MeV is studied by numerical simulations. The precipitating fluxes are formed as a result of both linear and nonlinear interaction; for energies 2-5 MeV precipitating fluxes are close to the strong diffusion limit. The evolution of precipitating fluxes is influenced by generation of higher-frequency waves at the packet trailing edge near the equator and dissipation of lower-frequency waves in the He+ cyclotron resonance region at the leading edge. The wave packet amplitude modulation leads to a significant change of precipitated particles energy spectrum during short intervals of less than 1 minute. For short time intervals about 10-15 s, the approximation of each local amplitude maximum of the wave packet by a Gaussian amplitude profile and a linear frequency drift gives a satisfactory description of the resonant interaction.


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