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A new phenomenon was found at the polar edge of the auroral oval in the
postmidnight - morning sectors: field-aligned (FA) high-energy upward electron
beams in the energy range 20 - 45 keV at altitudes about 3 RE,
accompanied by bidirectional electron FA beams of keV energy. The ILAT-MLT
location of the beams is consistent with a region of downward FA current
(Region I), although the exact correspondence is still not proved by direct
measurements. The beam intensity often reaches more than 104
electrons/s·sr·keV·cm2, and the beams are observed for a relatively
long time (~3·102-103 seconds), when the satellite
at the apogee moves slowly in the ILAT-MLT frame. A qualitative scenario
of the acceleration mechanism is proposed, according to which the satellite
is in between the bidirectional acceleration regions where a stochastic
FA acceleration is accomplished by waves with fluctuating FA electric field
components in both directions. The lower-hybrid, ion-cyclotron, ion-sound
waves, Langmuir and/or lower-hybrid cavitons, or ion holes, seem to be
possible candidates for such waves.
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