Grad-Shafranov reconstruction of a bipolar Bz signature in an earthward jet in the tail - PowerPoint PPT Presentation

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Grad-Shafranov reconstruction of a bipolar Bz signature in an earthward jet in the tail

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Grad-Shafranov reconstruction of a bipolar Bz signature in an ... associated with a substorm (onset at ~22:50 UT) 2002-08-13 Cluster event (2312-2318 UT) ... – PowerPoint PPT presentation

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Title: Grad-Shafranov reconstruction of a bipolar Bz signature in an earthward jet in the tail


1
Grad-Shafranov reconstruction of a bipolar Bz
signature in an earthward jet in the tail
  • Hiroshi Hasegawa
  • ISAS/JAXA
  • _at_Uppsala (2007/02/14)

2
Observation of bipolar Bz
to - Bz (GSM) in the mid- to distant-tail
along with tailward flows studied in
association with substorms (Ieda et al., 1998,
etc.)
3
Earthward moving flux rope? - to Bz often
seen in the near-tail (from Geotail and Cluster
observations).
Slavin et al. (2003)
4
Superposed epoch analysis
Core By field Observed along with earthward
flows (BBFs)
Slavin et al. (2003)
5
Models for bipolar Bz in earthward flows
Vz
Multiple X-line reconnection (forming magnetic
flux ropes) (e.g., Slavin et al., 2003)
Transient reconnection (e.g., Sergeev et al.,
1992) Localized reconnection under guide-field
By (Shirataka et al., 2006)
6
2002-08-13 Cluster event (2200-2400 UT)
Studied by Amm et al. (2006) associated with a
substorm (onset at 2250 UT)
7
2002-08-13 Cluster event (2312-2318 UT) -/ Bz
embedded in an earthward flow C3 exactly at
the center of the current sheet C1, 2, 4 on
the northern side Separation 4000 km
Bx
Bz
Vx
8
Grad-Shafranov reconstruction technique (Hau
Sonnerup, 1999) (A spatial initial value
problem) Assumptions Plasma structures are in
magnetohydrostatic equilibria (time-independent).
Magnetic field tension balances with force from
the gradient of total (magnetic plasma)
pressure.
2-D (no spatial gradient in the z
direction) Grad-Shafranov (GS) equation (e.g.,
Sturrock, 1994)
Pt, p, and Bz are functions of A alone (constant
on same field lines).
9
Reconstruction procedure
A 2D structure
Reconstruction plane
Y
Spatial integration
Y
VST_X
X
X
VST (VHT) (in the x-z plane)
Lx VST_X T (analyzed interval) X axis SC
trajectory in the x-y plane
Z (invariant axis)
10
Spatial initial value problem
(Sonnerup Guo, 1996)
Grad-Shafranov equation
spatial integration in -/ y direction
(2nd order Taylor exp.)
(1st order Taylor exp.)
GS eq.
11
z
x
cc 0.961
Roughly circular flux rope Flux rope with
half width of 1 Re Strong core field (mostly
By)
VHT (237, 27, 23) km/s in GSM i (-0.999,
0.042, 0.005) j (-0.022, -0.621, 0.784) k
(0.036, 0.783, 0.621)
Consistent with multiple X-line models?
12
3D-MHD simulation of localized reconnection with
guide-field (Shirataka et al., 2006)
guide-fieldBy0
The Northern hemisphere
2Ry
The plane of the equator
2Ry 3 Re
The Southern hemisphere
Slavin et al. 2003
13
Results
Reproducing the southward magnetic field
Shirataka et al. (2006)
14
Results
Virtual S/C obs. in the MHD run
Bz z0
11.25Re
By04nT, 2Ry3.0Re
t135s
15
Virtual observation vs real data
What will be reconstructed, when applied to the
simulation data in which no flux rope is created?
16
Virtual spacecraft observations _at_ (x,y,z)
(11.25, 0, 0), (11.25, 0, 1), (11.25, 1,
0), (11.25, 2, 0) Re Applied to the interval T
105 195 s (A suitable model may be
determined if the separation is 2Re. )
17
GS map recovered from virtual observation
Map recovered from data sampled at (x,y,z)
(11.25, 0, 0) Re
A flux rope, which does not really exist in the
simulation, is reconstructed erroneously.
Z(GS) (0.000, 0.996, 0.087)
18
Map recovered from data sampled at (x,y,z)
(11.25, 1, 0) Re
The presence of a flux rope-like structure in
GS maps does not necessarily mean that it exists
in reality. But, are GS results totally
meaningless?
19
Map recovered from data sampled at (x,y,z)
(11.25, 0, 0) Re
Simulation result at the time when Bz reversal is
at x11.25 Re (in the same plane)
20
Map recovered from data sampled at (x,y,z)
(11.25, 1, 0) Re
Simulation result at the time when Bz reversal is
at x11.25 Re (in the same plane)
21
Which model is more reasonable (for the Cluster
event)? CL event Roughly circular Pressure
minimum at the core
Simulation result Elongated in the x
direction Enhanced P at the front
22
Summary The GS method cannot accurately recover
the magnetic topology. One must be cautious
about interpretation of model-based (force-free,
or GS model) results. It seems possible to
get some information on the basic structure
(shape, pressure distribution, etc.) in the
reconstruction plane. The Cluster bipolar Bz
event on 2001-08-13 is most likely explained by a
flux rope (multiple X-line reconnection). A
suitable separation distance for discriminating
models is a few Re (comparable to the jet width).
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