Several mechanisms have been proposed as the cause of electron conics,
including perpendicular, oblique, and parallel heating, as well as ac
celeration by both stochastic and oscillating parallel electric fields
. While the conic distributions and various wave modes have been obser
ved together. been made of the actual acceleration mechanism while it
is in progress. This study reports on data obtained by DE-1, which mea
sured conics at high altitudes (greater than or equal to 10,000 km) ov
er the auroral oval, and DE-2, which simultaneously measured electron
distributions at low altitudes (similar to 900 km) in the same latitud
e/local time region. The DE-2 electron distributions often show the lo
w-altitude signature of a downward field-aligned beam, which has sprea
d to pitch angles of about 55 degrees as a result of the magnetic mirr
or force, along with an upward-moving electron conic distribution loca
lized in the same pitch-angle range. Even though the electron conics o
bserved by DE-2 have energies of only several hundred eV, compared to
the several keV conics observed by DE-1, these observations neverthele
ss support models in which field-aligned bursts and electron conics oc
cur on the same field line, with the conic being the result of the mag
netic mirroring of the part of the downward electron beam that lies ju
st outside the loss cone.