The purpose of this study is to investigate energy transfer processes in the Earth\u27s magnetotail. An equilibrium, two-dimensional magnetic field model is used to simulate the mid-tail region. Groups of particles are traced in the model magnetic field and the groups are combined to generate a self-consistent two-dimensional current sheet. Two thin current sheets are generated with thicknesses characteristic of a substorm growth phase. One current sheet contains Speiser-type particles only and the other one contains mostly Speiser-type and some trapped particles. It is found that the two current sheets show differences in energy flow processes and pressure anisotropies due to the different nature of orbits that they support. The generalize...
To investigate the energy involved by a substorm, we performed global magnetohydrodynamics simulatio...
The approximate magnitudes of several power inputs and energies associated with the Earth's magnetos...
Codes involving one and two spatial dimensions and three velocity dimensions were used to model the ...
The purpose of this study is to investigate energy transfer processes in the Earth\u27s magnetotail....
The purpose of this study is to investigate velocity space distribution functions in space plasmas. ...
Thick and thin models of the middle magnetotail were developed using a consistent orbit tracing tech...
The main thrust of our research is to study the consequences of particle dynamics in the current she...
The purpose of this study is to gain physical insight into how charged particles, that violate the g...
Physical processes in the Earth's magnetotail are investigated using data principally from the Plasm...
The auroral current density-voltage and energy flux density-voltage relationships are derived under ...
To advance our understanding of the magnetic storm dynamics of the outer radiation belt relativistic...
Dissertation (Ph.D.) University of Alaska Fairbanks, 1997A magnetofrictional method and MHD simulati...
International audienceThe influence of magnetic turbulence in the near-Earth magnetotail on ion moti...
Most of the work carried out to date on this project is summarized in the enclosed reprints of two p...
The magnetotail, the region of stretched magnetic field lines on the night side of the Earth, is imp...
To investigate the energy involved by a substorm, we performed global magnetohydrodynamics simulatio...
The approximate magnitudes of several power inputs and energies associated with the Earth's magnetos...
Codes involving one and two spatial dimensions and three velocity dimensions were used to model the ...
The purpose of this study is to investigate energy transfer processes in the Earth\u27s magnetotail....
The purpose of this study is to investigate velocity space distribution functions in space plasmas. ...
Thick and thin models of the middle magnetotail were developed using a consistent orbit tracing tech...
The main thrust of our research is to study the consequences of particle dynamics in the current she...
The purpose of this study is to gain physical insight into how charged particles, that violate the g...
Physical processes in the Earth's magnetotail are investigated using data principally from the Plasm...
The auroral current density-voltage and energy flux density-voltage relationships are derived under ...
To advance our understanding of the magnetic storm dynamics of the outer radiation belt relativistic...
Dissertation (Ph.D.) University of Alaska Fairbanks, 1997A magnetofrictional method and MHD simulati...
International audienceThe influence of magnetic turbulence in the near-Earth magnetotail on ion moti...
Most of the work carried out to date on this project is summarized in the enclosed reprints of two p...
The magnetotail, the region of stretched magnetic field lines on the night side of the Earth, is imp...
To investigate the energy involved by a substorm, we performed global magnetohydrodynamics simulatio...
The approximate magnitudes of several power inputs and energies associated with the Earth's magnetos...
Codes involving one and two spatial dimensions and three velocity dimensions were used to model the ...