AGU Fall Meeting, San Francisco, 15-19 December 1996
Abstract:
Ulysses' unique trajectory has enabled, for the first time, direct, accurate
and uninterrupted observation of a large number of Interplanetary Coronal
Mass Ejections (ICMEs) at a wide range of heliolatitudes. We have examined
the magnetic signatures of 57 ICMEs and compared their start and stop times
to the start and stop times as derived from the solar wind observations
(González-Esparza et al., 1996). We find that some magnetic signatures which
are clearly associated with the ICMEs precede the plasma ICME start time and
some extend beyond the plasma stop time. We have used both low variance and
a smooth field rotation as characterising the magnetic fields assocaited
with ICMEs. The statistics of the relationship between the durations in the
magnetic field and plasma signatures are presented. The internal magnetic
structure of an ICME is highlighted for one particular event - two ICMEs
occurring on July 16th, 1992 and July 24th, 1992. The ICMEs, between them,
are believed to have temporarily deflected the heliospheric current sheet
equatorward of its expected position (Balogh et al., 1993). A Minimum
Variance Analysis of the magnetic field in the first CME of the two reveals
two distinct magnetic regimes - a proposed cylindrical topology followed by
a region of constant, almost unidirectional magnetic field lines.