The density and temperature structure of the low-energy ion population
in the outer plasmasphere is examined by using data from Los Alamos N
ational Laboratory's three-dimensional magnetospheric plasma analyzer
at synchronous orbit. We define the ''outer plasmasphere'' as regions
of dense, cold plasma observed at synchronous orbit, with no attempt t
o distinguish between the main plasmasphere or detached plasma regions
existing beyond the plasmapause. We find that for moderate to high le
vels of geomagnetic activity the outer plasmasphere typically has a fi
ne-scale density structure. The amount of variability in the density g
enerally increases with increasing geomagnetic activity, as indicated
by Kp, and the most variable intervals are associated with substorm ac
tivity. The dense (>10 ions cm(-3)), cold (approximate to 1 eV), plasm
aspherelike plasma is adjacent to, and often interspersed with, low-de
nsity (1-10 ions cm(-3)), warm (2-10 eV), ''troughlike'' plasma region
s. We find that occasionally these two temperature populations can coe
xist, but that most often they do not. The scale size of the fine-scal
e structure in the dense, cold plasma regions often is of the order of
1000 km or less, These observations suggest that fine-scale density s
tructure in the dusk sector of the outer plasmasphere is imposed by pe
netrating substorm electric fields.