The acceleration of magnetospheric electrons to multi-MeV energies has been
a topic of much interest and study over the last several years. To further
investigate this acceleration process, Polar and SAMPEX data from 1997 and
1998 were used to examine the general, repeating characteristics of the re
lativistic electron injection events that occurred over the 2-year period.
Around the intensity peak, usually in the L range from 3.2 to 4.5, it was f
ound that (1) during the main phase of the storm, there is a dropout of the
relativistic electron fluxes; (2) fluxes increase as recovery begins; (3)
the electrons are most sharply peaked in pitch angle at the beginning of th
e event and flatten with time; (4) the rate at which the flux increases slo
ws with increasing energy; and (5) strong pitch angle scattering is intimat
ely associated with relativistic electron injection events. A recirculation
or resonant heating process coupled with rapid radial diffusion or a meldi
ng of both would be consistent with the observations.