5. Charge excess in Auroral zones at high altitude
(André Mangeney)
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PHYSICAL PROBLEM: What is the
origin of the localized electron excesses (or
"electrostatic bipolar structures") observed at high altitudes in the auroral
zones?
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OBSERVATIONS: in the polar
auroral zones by FAST,
FREJA (spacecrafts on terrestrial orbits measuring waveforms for the electric
potential); similar wave forms
are observed in the solar wind (here the Wind mission)
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EQUATIONS:
Vlasov
equation for a strongly magnetized plasma (particles move along
the magnetic field; the electic field depends on two spatial
coordinates, parallel and perpendicular to the field)
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NUMERICAL EXPERIMENTS: One starts
from a plasma with uniform electron density
but made of two electron populations with opposite velocities (mimicking
the auroral population). The boundaries of the domain are open.
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CONCLUSION: the two populations
are unstable, and the density does not remain uniform; electron packets
are generated corresponding to the observed "bipolar structures".
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REFERENCE: work in progress...
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5. auroral zones (continued)
The FILM (mov,
4 Mb; gif, 2,9 Mb)
shows the plasma evolution starting from two electron populations with
opposite velocities but with uniform density.
The initial homogeneous state changes rapidly: fluctuations
of the electronic density appear.
Two phases show up:
a) The linear phase, during which the fluctuations grow
(oblique strips which then undergo fragmentation)
b) The saturation phase, during which sporadic, intermittent
electron blobs appear.
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