This study examines substorm-associated magnetic field fluctuations ob
served by the AMPTE/CCE and SCATHA satellites in the near-Earth tail.
Three tail reconfiguration events are selected, one event on August 28
, 1986, and two consecutive events on August 30, 1986. The fractal ana
lysis was applied to magnetic field measurements of each satellite. Th
e result indicates that (1) the-amplitude of the fluctuation of the no
rth-south magnetic component is larger, though not overwhelmingly, tha
n the amplitudes of the other two components ana (2) the magnetic fluc
tuations do have a characteristic timescale, which is several times th
e proton gyroperiod. In the examined events the satellite separation w
as less than 10 times the proton gyroradius. Nevertheless, the compari
son between the AMPTE/CCE and SCATHA observations indicates that (3) t
here was a noticeable time delay between the onsets of the magnetic fl
uctuations' at the two satellite positions, which is too long to ascri
be to the propagation of a fast magnetosonic wave, End (4) the coheren
ce of the magnetic fluctuations was low in the August 28, 1986, event
and the fluctuations had different characteristic timescales in the fi
rst event of August 30, 1986, whereas some similarities can be found f
or the second event of August 30, 1986. Result 1 indicates that pertur
bation electric currents associated with the magnetic fluctuations ten
d to flow parallel to the tail current sheet and are presumably relate
d to the reduction of the tail current intensity. Results 2 and 3 sugg
est that the excitation of the magnetic fluctuations;and therefore the
trigger of the tail current disruption is a kinetic process in which
ions play an important role. It is inferred from results 3 and 4 that
the characteristic spatial scale of the associated instability is of t
he order of the proton gyroradius or even shorter, and therefore the t
ail current disruption is described as a system of chaotic filamentary
electric currents. However, result 4 suggests that the nature of the
tail current disruption can vary from event to event.