NearEarth Magnetotail Reconnection and Plasmoid Formation in Connection With a Substorm Onset on 27 - PowerPoint PPT Presentation

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Title: NearEarth Magnetotail Reconnection and Plasmoid Formation in Connection With a Substorm Onset on 27


1
Near-Earth Magnetotail Reconnection and Plasmoid
Formation in Connection With a Substorm Onset on
27 August 2001
  • S. Eriksson1, M. Oieroset2, D. N. Baker1, C.
    Mouikis3,
  • M. W. Dunlop4, H. Reme5, R. E. Ergun1, and A.
    Balogh6
  • 1 Laboratory for Atmospheric and Space Physics,
    University of Colorado at Boulder, USA
  • 2 Space Sciences Laboratory, University of
    California at Berkeley, USA
  • 3 Space Science Center, University of New
    Hampshire, USA
  • 4 Rutherford Appleton Laboratory, UK
  • 5 Centre dEtude Spatiale des Rayonnements,
    France
  • 6 Imperial College, UK

Contact information eriksson_at_lasp.colorado.edu
2
Outline
  • Introduction
  • Tail reconnection and slow-mode shocks
  • deHoffmann-Teller and Walen analyses
  • Cluster observations and Walen analyses
  • August 27 2001 from 0350 UT to 0435 UT
  • (post-midnight event)
  • Summary

3
Tail Reconnection and Slow-mode Shocks
Hill, T.W., JGR, 80, 4689, 1975
Feldman et al., JGR, 92, 83, 1987
  • Acceleration in tail reconnection is assumed to
    take place across a slow-mode shock connected to
    the diffusion region. Configuration essentially
    that of Petschek 1964 (above right).

4
Tail Reconnection and Slow-mode Shocks
Hill, T.W., JGR, 80, 4689, 1975
Feldman et al., JGR, 92, 83, 1987
  • Slow-mode shocks are defined in ideal MHD by an
    increased plasma pressure and a decreased B-field
    strength where the B-field bends toward the shock
    normal.

5
Tail Reconnection and Slow-mode Shocks
Hill, T.W., JGR, 80, 4689, 1975
Feldman et al., JGR, 92, 83, 1987
  • Slow-mode shocks were first observed in the
    tail by e.g. Feldman et al. 1984, 1987 using
    the Rankine-Hugoniot jump conditions. Also
    suggested by Oieroset et al. 2000 who
    successfully used the Walen analysis on Wind data
    60 Re downtail.

6
deHoffmann-Teller Analysis
Khrabrov and Sonnerup, ISSI Sci.rep., 1998
  • The existence of an HT frame indicates the
    presence of a quasi-stationary coherent pattern
    of magnetic field and plasma velocity. The HT
    interval should include data points on either
    side of the boundary.

7
deHoffmann-Teller Analysis
Khrabrov and Sonnerup, ISSI Sci.rep., 1998
  • A Galilean HT frame transformation allows for
    the identification and analysis of such coherent
    structures (e.g. slow-mode shocks) moving past an
    observing platform.

8
Walen Analysis as a Test of Reconnection
(Not a slow shock since B does not bend toward
normal)
  • Reconnection predicts that the generated
    rotational discontinuity (finite normal B-field
    component) propagates away from the diffusion
    region at a field-aligned phase speed in the HT
    shock frame and its magnitude is determined by
    the type and strength of the shock.

9
Walen Analysis as a Test of Reconnection
(Not a slow shock since B does not bend toward
normal)
  • The sign of the Walen slope depends on whether
    the B-field is parallel or antiparallel to the
    flow direction.

10
Walen Analysis in the Magnetotail
Walen slope
Oieroset et al., JGR, 105, 25,247, 2000.
  • Region I earthward jet, Bxgt0, RWlt0
  • Region II tailward jet, Bxgt0, RWgt0

11
Walen Analyses at Wind (x -60 Re)
Oieroset et al., JGR, 105, 25,247, 2000.
  • Earthward jet interval
  • Negative Bx
  • Walen slope should be positive

Note that there is no ion composition in the Wind
data set and that these slopes were derived
assuming 100 H.
12
Cluster Location August 27 2001
13
Cluster Observations on August 27 2001
Density (CODIF)
Plasma b (CODIF)
A
B
C
Ion speed (HIA)
Vx, Vy, Vz
Bx, By, Bz
Magnetic field magnitude
Alfven Mach number Note MAlt1
14
Cluster Observations on August 27 2001
Density (CODIF)
Plasma b (CODIF)
A
B
C
Ion speed (HIA)
Vx, Vy, Vz
Bx, By, Bz
Magnetic field magnitude
Approximate substorm onset in global UV images at
0406-0408 UT Baker et al., GRL, 2002
Alfven Mach number Note MAlt1
15
Comparison with the Substorm of April 24 1979
Bx
Bx
sc1 sc3
Overview of ISEE 2 magnetic field (GSE) and
plasma data near substorm onset. H
ones et al.,1986 Feldman et al., 1987
By
By
Bz
Bz
Pp
beta
Vx
Vx
16
Comparison with the Plasmoid of April 24 1979
Cluster magnetic field hodogram (GSM)
Three-dimensional magnetic field structure of
plasmoid at substorm onset from Hones et al.,
GRL, 1982.
17
Walen Analyses on August 27 2001(A) Tailward
Region II Jets 0400-0403 UT
sc1
  • Positive Bx
  • Tailward jets
  • Prediction
  • Positive Region II
  • Walen slope

sc3
18
Walen Analyses on August 27 2001(B) Earthward
Region I Jets 0406-0410 UT
  • Positive Bx
  • Earthward jets
  • Prediction
  • Negative Region I
  • Walen slope

sc1 0406-0408 UT
sc3 0409-0410 UT
19
Walen Analyses on August 27 2001(C) Earthward
Region I Jets 0426-0428 UT
sc1
  • Positive Bx
  • Earthward jets
  • Prediction
  • Negative Region I
  • Walen slope

sc3
20
B
A
C
x black y green z red
Angle between V and B .
21
Substorm of 27 August 2001
(A)
22
Substorm of 27 August 2001
(B)
23
Substorm of 27 August 2001
(B)
(C)
24
Note on Importance of Density for the Walen Slope
A mix of 5 O ions and 95 H results in an
effective mass m1.75mp and a lower Alfven speed,
that effectively should increase the Walen slope
.
25
Impact of mmp Assumption
O fraction 0.8 - 4.8 Avg O fraction
1.8 Walen slope0.73
Assume 100 H Walen slope0.65
26
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27
Summary
  • The Walen test together with the location of
    Cluster north of the neutral sheet confirms the
    presence of a slow mode shock on the tailward
    side of the near-Earth X-line on August 27, 2001
    that most likely accelerated the ions.
  • The Walen test for some earthward jets may
    indicate a correct slope (sign), although the
    quality of the HT frame is lower.
  • The earthward jets seem to be more field-aligned
    which implies that ideal MHD (and thus the HT
    analysis) breaks down.
  • The use of ion composition data from CODIF
    improved the Walen slope.
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