The temporal and spatial scales of the onset of two types of substorm
events are investigated. These substorms were cases where the expansio
n onset had precursor localized auroral activation without significant
negative bay enhancement, that is, ''pseudobreakup''. High-resolution
energetic particle and magnetic field data at synchronous orbit are u
sed for the analysis together with auroral and magnetic field data sim
ultaneously taken from ground-based instrumentation. The auroral struc
ture following the pseudobreakup significantly resembled the major exp
ansion aurora, except in its spatial scale. Typical magnetospheric ons
et signatures such as tail current diversion, dipolarization, and inje
ction were observed associated with some of the pseudobreakups. The ma
jor expansion, on the other hand, consisted of a number of rather loca
lized injection and expansions, each of which had timescales of 2-8 mi
n, a comparable timescale to that of pseudobreakups. This study shows
that there does not appear to be any phenomenological differences betw
een pseudobreakups and major expansion onsets. The major difference be
tween pseudobreakups and major expansion onsets would be the number of
occurrences, as well as the intensity and the scale size of the magne
tospheric source.