Typical electron velocity distribution functions observed at 1 AU from the
Sun by the 3DP instrument onboard Wind are used as boundary conditions to d
etermine the electron velocity distribution function at 4 solar radii in th
e corona. The velocity distribution functions (VDFs) at low altitude are ob
tained by solving the Fokker-Planck equation, using two different sets of b
oundary conditions. The first set typically corresponds to a VDF observed i
n a low-speed solar wind flow (i.e., characterized by "core" and "halo" ele
ctrons); the second one corresponds to highspeed solar wind (i.e., characte
rized by "core," "halo,", and "strahl" populations). We use the observed el
ectron VDFs as test particles, which are submitted to external forces and C
oulomb collisions with a background plasma. Closer to the Sun, the relative
density of the core electrons is found to increase compared to the density
of the halo population. Nevertheless, we find that in order to match the o
bserved distributions at 1 AU, suprathermal tails have to be present in the
VDF of the test electron at low altitudes in the corona.