We have studied possible braking mechanisms of high-speed ion flows in
the near-Earth central plasma sheet for radial distances between 9 an
d 19 Earth Radii (R-E) on the basis of observations made by the AMPTE/
IRM satellite. Flows with velocities in excess of 400 km/s are almost
always Earthward for this range, indicating that the source of the flo
ws is beyond 19 R-E. Though the occurrence rate of the highspeed flows
substantially decreases when the satellite comes closer to the Earth,
high-speed flows with velocities higher than 600 km/s are still obser
ved. We suggest that the high-speed flows are stopped at a clear bound
ary between the regions of dipolar field and tail-like field in the pl
asma sheet. The boundary corresponds to the inner edge of the neutral
sheet. The average jump of the magnetic field at the boundary, which i
s estimated from the observations by assuming a pressure balance, is 6
.7 nT. The inertia current caused by the braking of the flow and the c
urrent caused by pileup of the magnetic flux at the stopping point are
quantitatively estimated and discussed in relation to the formation o
f the substorm current wedge.