The interval of 1997 January 1-2 was identified as a favorable conjunction
of Geotail and IMP-8 to examine substorm activity in the mid-tail region pr
ior to data acquisition. On January 2, 1997, global auroral observations fr
om Polar indicated a substorm onset at similar to 0120 UT followed by a sub
storm intensification at similar to 0154 UT sit a local time spatially sepa
rated from the initial substorm activity region. During this event, both Ge
otail and IMP-8 were in the mid-tail near the midnight meridian (Geotail (X
, Y) approximate to (-30,-3)R-E and IMP-8 (X,Y) approximate to (-37,2)R-E).
Observations indicated that the substorm onset activity was localized in t
he postmidnight region. After the onset, Geotail detected a transient dipol
arization which was not accompanied by large plasma flows (i.e., \ V-x \les
s than or equal to 200 km/s). The subsequent substorm intensification produ
ced enduring dipolarization at Geotail and highly fluctuating magnetic fiel
d (mostly northward B-z) at IMP-8. Observations for this substorm showed no
indication of mid-tail activities occurring prior to auroral brightening f
or both onset and intensification even though the satellites observed activ
ities subsequently. Close examination of data indicates that the delays wer
e not due to a dawn-dusk expansion of mid-tail activity. These results are
consistent with substorm activity beginning in the near-Earth region first,
followed by activity in the mid-tail region later.