The AMPTE CCE satellite frequently observed transient (1 less than or
equal to tau less than or equal to 8 min) events marked by magnetic fi
eld strength increases and bipolar magnetic field signatures peak-to-p
eak amplitudes greater than or equal to 4 nT) while in the outer daysi
de magnetosphere. We report a survey of 59 prominant events observed f
rom August to November 1984. The bipolar signatures and minimum varian
ce analysis reveal that most events move poleward and antisunward, exc
ept in the immediate vicinity of local noon. Here the motion of the ev
ents appears to be better governed by the spiral/orthospiral interplan
etary magnetic field (IMF) orientation than magnetic curvature forces
associated with IMF B-y. The IMF orientation appears to have little or
no influence on event occurrence or orientation. We interpret the eve
nts in terms of solar wind/foreshock pressure pulse induced ripples on
the magnetopause surface. Our results can be reconciled with those ob
tained in previous studies which made use of ISEE 1/2, AMPTE IRM, and
AMPTE UKS observations if pressure pulses produce large-amplitude even
ts and bursty merging (or reconnection) produces small-amplitude event
s.