Dn. Baker et al., RELATIVISTIC ELECTRON ACCELERATION AND DECAY TIME SCALES IN THE INNERAND OUTER RADIATION BELTS - SAMPEX, Geophysical research letters, 21(6), 1994, pp. 409-412
High-energy electrons have been measured systematically in a low-altit
ude (520 x 675 km), nearly polar (inclination = 82-degrees) orbit by s
ensitive instruments onboard the Solar, Anomalous, and Magnetospheric
Particle Explorer (SAMPEX). Count rate channels with electron energy t
hresholds ranging from 0.4 MeV to 3.5 MeV in three different instrumen
ts have been used to examine relativistic electron variations as a fun
ction of L-shell parameter and time. A long run of essentially continu
ous data (July 1992 - July 1993) shows substantial acceleration of ene
rgetic electrons throughout much of the magnetosphere on rapid time sc
ales. This acceleration appears to be due to solar wind velocity enhan
cements and is surprisingly large in that the radiation belt ''slot''
region often is filled temporarily and electron fluxes are strongly en
hanced even at very low L-values (L approximately 2). A superposed epo
ch analysis shows that electron fluxes rise rapidly for 2.5 less than
or similar L less than or similar 5. These increases occur on a time s
cale of order 1-2 days and are most abrupt for L-values near 3. The te
mporal decay rate of the fluxes is dependent on energy and L-value and
may be described by J = Ke-t/to with t(O) almost-equal-to 5-10 days.
Thus, these results suggest that the Earth's magnetosphere is a cosmic
electron accelerator of substantial strength and efficiency.