Acceleration of hydrogen ions and conic formation along auroral field lines
Electrostatic ion cyclotron turbulence and the formation of ion conics at low altitudes (approx. = 1500 km) along auroral field lines have been investigated analytically and by plasma numerical simulations. Ion cyclotron waves are assumed to be driven unstable by the up-going cold ionospheric electrons associated with the downward auroral current. When the electron drift speed is comparable to the electron thermal speed, it is found that the large amplitude, e phi/T/sub e/ approx. = 1, coherent, ..omega.. = ..cap omega../sub i/, ion cyclotron waves shoudl exist along auroral field lines at low altitudes extending approx. = 500 to 1000 km. Ion conics are associated with the cyclotron turbulence and the ion bulk temperature is found to increase a factor of 10 of the initial ionospheric temperature, while the temperature of the high energy tail can be as much as a factor of 100 of the ionospheric temperature. Theory and simulations agree well.
- Research Organization:
- Princeton Univ., NJ (USA). Plasma Physics Lab.
- DOE Contract Number:
- AC02-76CH03073
- OSTI ID:
- 5233921
- Report Number(s):
- PPPL-1902; ON: DE82016685
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
640201* -- Atmospheric Physics-- Auroral
Ionospheric
& Magetospheric Phenomena
71 CLASSICAL AND QUANTUM MECHANICS
GENERAL PHYSICS
ACCELERATION
AURORAE
CHARGED PARTICLES
CYCLOTRON FREQUENCY
EARTH ATMOSPHERE
GEOMAGNETIC FIELD
HYDROGEN IONS
ION DRIFT
IONOSPHERE
IONS
MAGNETIC FIELDS
PLANETARY IONOSPHERES
TURBULENCE
Ionospheric
& Magetospheric Phenomena
71 CLASSICAL AND QUANTUM MECHANICS
GENERAL PHYSICS
ACCELERATION
AURORAE
CHARGED PARTICLES
CYCLOTRON FREQUENCY
EARTH ATMOSPHERE
GEOMAGNETIC FIELD
HYDROGEN IONS
ION DRIFT
IONOSPHERE
IONS
MAGNETIC FIELDS
PLANETARY IONOSPHERES
TURBULENCE