Dipolarization of the earth magnetic field and charge particles precipitation from the magnetic flux tube
During the expansion phase of the substorm in the nightside magnetosphere enhancement of the magnetic field and decrease the plasma pressure is observed simultaneously. Enhancement of the magnetic field is recorded at first in the tail of the magnetosphere, and then at more closer distances from the Earth. This ...
Non-stationary polar wind in presence of magnetosphere convection
Time-depended hydrodynamic model TUBE 7 is used for modeling of field-aligned motions and temperature of polar ionosphere ions taking into account magnetosphere convection. It was shown tube geometry changing have a great influence on basic parameters of polar magnetosphere thermal plasma.
1.
Banks P. M., Holzer
Т
.
Е
.
The polar wind // J. Geophys. Res. 1968. Vol. 73, №
21. P. 6846—6854....
Simulating of non-stationary processes in the ionospheric plasma
... The article presents numerical calculation results of variations of charged particles concentration in the ionosphere and the plasmasphere. The comparative analysis of various hydrodynamic approximations for the description of the ionospheric and the magnetospheric plasma is carried out. It is made on the basis of the numerical solution of the system of equations of energy, continuity and motion for O+, H+ ions and electrons along a power tube of the geomagnetic field. Differences between the hydrodynamic ...
Dynamical anthropogenic perturbations of ionosphere-magnetospheric plasma
... Математическое моделирование.
1989.
Т
. 1, №
8.
С
. 83—98.
10.
Hedin A. E.
Thermospheric model // J. Geophys. Res. 1987. V
ol
. 92, №
A
5.
P
.
4649—4662.
Ishanov S. A.
simulation, anthropogenic perturbation, ionosphere, magnetosphere, plasma.
33-41