Three-dimensional magnetic field structure in the inner magnetosphere
is statistically analyzed using data obtained by the DE-1 magnetometer
. The main results are as follows: (1) The magnetic field. structure o
f the rotational pattern associated with an eastward current is clearl
y seen in the dayside equatorial region at geocentric distances around
2.5R(e) but not on the nightside, The current density is approximatel
y 0.05 mu A/m(2), and does not show any clear dependence on geomagneti
c disturbance, but shows a solar activity dependence which possibly su
ggests that a substantial part of the closure of the eastward current
is through the dayside mid-latitude ionosphere, (2) The azimuthal comp
onent of the magnetic field associated with field-aligned currents is
seen in the low-latitude magnetosphere, The intensity of this componen
t is about 5 to 10 nT, and has a dependence on geomagnetic activity, (
3) Compared with the currently available magnetospheric models, the ob
served inner magnetospheric magnetic fields have much more complex str
uctures than the models indicate, The necessity of including the field
-aligned current system and an eastward current in the models is evide
nt, (4) A noon-midnight asymmetry of tile magnetic structure is clearl
y seen, particularly in the southward component associated with the ri
ng current, The asymmetry is much larger in this meridian than that in
the dawn-dusk meridian, This is in contrast with the asymmetry observ
ed on the ground or by low-altitude satellites over the ionosphere.