Fig' 3a and 3b' Cluster FGM Balogh et al', 2001, CIS Reme et al', 2001 and PEACE Johnstone et al', 1 - PowerPoint PPT Presentation

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Fig' 3a and 3b' Cluster FGM Balogh et al', 2001, CIS Reme et al', 2001 and PEACE Johnstone et al', 1

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Title: Fig' 3a and 3b' Cluster FGM Balogh et al', 2001, CIS Reme et al', 2001 and PEACE Johnstone et al', 1


1
Cluster observations of flux rope structures in
the near-tail
P. D. Henderson1, C. J. Owen1, I. V. Alexeev1, J.
Slavin2, A. N. Fazakerley1, E. Lucek3, and H.
Reme4
1Mullard Space Science Laboratory, University
College London, Holmbury St. Mary, Dorking, UK,
RH5 6NT 2Laboratory for Extraterrestrial Physics,
NASA GSFC, Greenbelt, MD, USA, 20771 3Space and
Atmospheric Physics, Imperial College London, UK,
SW7 2BZ 4Centre d'Etude Spatiale des
Rayonnements, Toulouse, France
Abstract An investigation of the 2003 Cluster
tail season has revealed small flux ropes in the
near-tail plasma sheet of Earth. Two flux ropes
are detailed in this poster, observed on the 2nd
October and on the 13th August 2003. The flux
rope observed on the 2nd October was travelling
Earthward and duskward at 160 kms-1. The axis
was close to the intermediate variance direction
of the magnetic field. Throughout the flux rope,
but more significant in the outer sections, J ? B
was large. The components of J ? B suggest that
the magnetic force was acting to radially expand
the flux rope, i.e. directed away from the centre
of the flux rope. The flux rope observed on the
13th August was travelling tailward at 200 kms-1.
The axis was directed close to the maximum
variance direction of the magnetic field. J ? B
was larger in the outer sections of the flux rope
than in the centre. This flux rope was also under
expansive magnetic pressure forces from J ? B,
i.e. directed away from the centre of the flux
rope. Electron pressure was reduced inside the
flux ropes, suggesting a compressional force from
the plasma. The observations of a large J ? B
signature in the outer sections of the flux ropes
may be explained if they are being observed at an
intermediate stage in their evolution from
creation by reconnection at multiple X lines near
the Cluster apogee towards the force-free like
configuration often observed further down the
tail. The centre of the flux ropes may contain
older reconnected flux at a later evolutionary
stage and may therefore be more force-free.
Fig 5a. Schematic representation of the results
shown graphically in Figs 3a and 4a.
Results
The magnetic force in both of these flux ropes
was magnetic pressure dominated, acting to
radially expand the flux ropes. The magnetic
force was smaller in the centre of the flux ropes
(Figs 4a and 4b). The electron pressure was
reduced inside the flux ropes, suggesting a
compressional force from the surrounding plasma
Introduction Flux ropes have been interpreted as
evidence for multiple X line reconnection (MXR)
in the near-tail associated with substorms (e.g.
Slavin et al., 2003). In MXR, instead of creating
one single X line in the tail, the conditions
required for reconnection can be satisfied in
numerous places, creating a number of X lines.
Given an IMF BY component which penetrates into
the tail, flux ropes can be created between the X
lines. Reconnection propagates out to open field
lines in the lobe, eventually leading to one
single magnetotail X line. The newly-formed flux
ropes are therefore embedded in Alfvenic jets
from the single X line and thus move away from
the point at which they were created. Flux ropes
are characterised by a bipolar BZ signature and a
large increase in the magnitude of B. Events with
a south-then-north (north-then-south) signature
are seen to move Earthward (tailward), and are
usually embedded in fast plasma flows Slavin et
al. (2003).
Fig 5b. Schematic representation of the results
shown graphically in Figs 3b and 4b.
Fig. 3a and 3b. Cluster FGM (Balogh et al.,
2001), CIS (Reme et al., 2001) and PEACE
(Johnstone et al., 1997) observations from 2nd
October and 13th August 2003. The flux ropes,
marked between two black lines, are embedded in
fast plasma flows observed from CIS. A high
plasma ion ß and large differential energy flux
of 1 keV electrons from CIS and PEACE
respectively show that the Cluster spacecraft
were deep within the plasma sheet.
Discussion The mechanism for the creation of
these structures is important for the study of
the break-up of current sheets near substorm
onset. The flux ropes reported on here are not
force-free, indeed tending to be less force-free
in the outer sections of the flux rope than in
the centre. As is the case for those seen in the
distant tail, the cores of these flux ropes would
perhaps be expected to relax into the constant a
force-free flux rope state, the lowest energy
state of a helical magnetic field, after some
time. If the process responsible for the creation
of these flux ropes is multiple X point
reconnection and if it is occurring close to the
point where the flux ropes are observed, the flux
ropes might not have had time to fully relax into
this force-free state. However, as the flux in
the centre of the flux ropes would have
reconnected before that in the outer sections,
the central flux would have had more time to
begin the evolution towards a force-free
configuration. The outer sections would therefore
be expected to less force-free than the centre,
as observed in both flux ropes reported here.
Fig. 1. The topology of a force-free helical flux
rope. A cartoon spacecraft trajectory is marked,
along with the variance coordinate system that
would arise from a force-free flux rope.
  • Conclusions
  • Conspicuously few well-formed flux ropes were
    found in the 2003 Cluster tail season.
  • Both flux ropes investigated here were found not
    to be in a force-free configuration, demonstrated
    by the computation of the J ? B forces inside the
    flux ropes.
  • J ? B was larger in the outer sections and
    magnetic pressure dominated in both flux ropes.
  • Electron pressure was reduced inside the flux
    ropes suggesting a compressional force from the
    plasma.
  • Flux rope axes do not always correspond to the
    intermediate variance direction of the magnetic
    field (as is the case for a simple force free
    flux rope), in one case the axis is close to the
    maximum variance direction.
  • Flux rope bipolar signatures were small (
    0.3RE) and slow moving ( 200 kms-1) , determined
    with multi-spacecraft timing and CIS ion moments.
  • Observation of a tailward moving flux rope at X
    (GSM) -18RE suggests that multiple X line
    reconnection must have occurred Earthwards of
    this point.

The simplest flux rope model is the force-free
flux rope (Fig. 1). This model represents the
minimum energy state for helical magnetic field
lines and could therefore represent the cores of
well developed, fully evolved flux ropes observed
in the deep tail.
Minimum variance analysis has previously been
used to determine the orientation of flux ropes.
For the force-free model above, a variance
analysis on the magnetic field gives an
intermediate variance direction which corresponds
to the axis of the flux rope (Xiao et al,. 2004).
The minimum variance direction will lie along the
trajectory (Fig. 1). By noting the time at which
different spacecraft measure the same level of
B, multi-spacecraft timing can be used to
construct moving planar surfaces to approximate
the curved outer boundaries of the flux ropes
(Fig. 2). The produced timing vectors define a
plane whose normal is the axis of the structure.
This can be used to estimate the axial
orientation of flux ropes.
References Balogh, A., et al., The Cluster
Magnetic Field Investigation overview of
in-flight performance and initial results, Ann
Geophys., 19, 1207, 2001. Dunlop, M. W., et al.,
Four-point cluster application of magnetic field
analysis tools The Curlometer, J Geophys. Res.,
107, 1384, 2002. Johnstone, A.D., et al., PEACE
A Plasma Electron And Current Experiment, Space
Sci. Rev, 79, 351, 1997. Reme, H., et al., First
multispacecraft ion measurements in and near the
Earths magnetosphere with the identical Cluster
ion spectrometry (CIS) experiment, Ann, Geophys.,
19, 1303, 2001. Slavin, J. A., et al., Geotail
observations of magnetic flux ropes in the plasma
sheet, J. Geophys. Res., 108, 1015, 2003. Xiao,
C. J., et al., Inferring of flux rope orientation
with the minimum variance technique, J. Geophys.
Res., 109, A11218, 2004.
In 2003 the separation of the Cluster spacecraft
was only 200 km. This small separation means that
the curolmeter technique (Dunlop et al., 2002)
can be used to determine the internal current
systems in small flux ropes observed in the
near-tail region. With knowledge of the current,
the magnetic force, J ? B, can be calculated.
This can then be resolved into magnetic tension
and pressure forces.
Fig. 4a and 4b. Current (J? and J, minimum
variance coordinates and J), relative
curlometer error, magnetic forces (pressure - red
and tension - blue in minimum variance
coordinates), electron pressure and magnetic
field observations (BZ and B) from 2nd October
flux rope, and 13th August flux rope
respectively.
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