Mh. Boehm et al., FREJA OBSERVATIONS OF NARROW INVERTED-V ELECTRON-PRECIPITATION BY THE2-DIMENSIONAL ELECTRON SPECTROMETER, Geophysical research letters, 21(17), 1994, pp. 1895-1898
Observations of several steady, approximately 1-5 km scale inverted-V'
s by the Freja F7 Two-dimensional Electron Spectrometer (TESP) are des
cribed. Such narrow structures are not common, but provide an opportun
ity for observing edge precipitation and the movement of arcs through
the plasma. Velocities of inverted-V potential structures in the plasm
a frame can be derived from the observed time delay between precipitat
ing and mirrored electrons. These velocities determine whether horizon
tal plasma flow into a potential structure can provide the source popu
lation for arc edge precipitation. It is found that the intensity of t
he arc edge precipitation is not associated in any expected way with t
his velocity, indicating another source of plasma for arc edge precipi
tation is required.