Data from sensors on board the Polar, Solar, Anomalous, and Magnetospheric
Particle Explorer (SAMPEX), and other Earth-orbiting spacecraft show that h
igh-energy electron intensities vary in a global, coherent way throughout t
he outer trapping zone of the terrestrial magnetosphere. Long-term measurem
ents of very energetic trapped electrons provide a comprehensive view of th
e large variability of intensities on timescales less than I day to times c
orresponding to the 11-year sun-spot cycle. The average density of relativi
stic electrons within the outer magnetospheric trapping region (2.5 <L <6.5
) is calculated in this paper during a 7-year observing period. The total e
nergy content and power dissipation in this relativistic electron component
are then compared on a yearly basis to the solar wind energy that impacts
the magnetosphere during the same time. The overall efficiency of relativis
tic electron production is thereby computed and is found consistently to be
similar to1% throughout the entire observing interval. Such efficiencies a
re important and potentially useful in scaling electron acceleration in oth
er, more remote solar, planetary, and cosmic systems. The results presented
here suggest that a range of different processes are involved in producing
very energetic electrons in various astrophysical plasmas.