Dg. Sibeck et Pt. Newell, INTERPLANETARY MAGNETIC-FIELD ORIENTATION FOR TRANSIENT EVENTS IN THEOUTER MAGNETOSPHERE, J GEO R-S P, 100(A1), 1995, pp. 175-183
It is generally believed that flux transfer events (FTEs) in the outer
dayside magnetosphere, usually identified by transient (similar to 1
min) bipolar magnetic field perturbations in the direction normal to t
he nominal magnetopause, occur when the magnetosheath magnetic field h
as a southward component. We compare the results of three methods for
determining the magnetosheath magnetic field orientation at the times
of previously identified UKS/IRM events: (I) the average magnetosheath
magnetic field orientation in the 30-min period adjacent to the neare
st magnetopause crossing, (2) the magnetosheath magnetic field orienta
tion observed just outside the magnetopause, and (3) the lagged interp
lanetary magnetic field (IMF) orientation at the time of the transient
events. Whereas the results of method 2 indicate that the events tend
to occur for a southward magnetosheath magnetic field, the results of
methods 1 and 3 show no such tendency. The fact that the three method
s yield significantly different results emphasizes the need for cautio
n in future studies.