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January 19, 2011 Construction of Magnetic Reconnection in the near-Earth Magnetotail with Geotail T. NagaiTokyo Institute of Technology I. ShinoharaISAS/JAXA. MHD Picture of Magnetic Reconnection. inflow. outflow. Bz > 0 Bz < 0. - PowerPoint PPT Presentation
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January 19, 2011
Construction of Magnetic Reconnection in the near-Earth Magnetotail with Geotail
T. Nagai Tokyo Institute of TechnologyI. Shinohara ISAS/JAXA
119:47
MHD Picture of Magnetic Reconnection
inflow
outflowBz > 0 Bz < 0
219:47
Ion flows
Electron flows
unit ViA
unit VeA
Particle Picture of Magnetic Reconnection
319:47
Hall Magnetic Fields
419:47
Ve Ve
Vi Vi
Outflows
Bz > 0 Bz < 0
MHD Ion-electron decoupling MHD
519:47
- Vey
electron current layer
Bz > 0 Bz < 0
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15 May 2003
near 1055 UT
the spacecraftGeotail at 28 RE
in situ observations ofmagnetic reconnection
Geotail
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Tailward flows
Earthward flows
Bz < 0 Bz > 0
Tailward flows
Earthward flows
Ion Et
Bz > 0 Bz < 0
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Main Targets of This Paper
1. Detect the central intense electron current layer2. Get scales of magnetic reconnection
with Geotail observations
VA = 2,200 km/s i = 1,200 km (ion inertial length)
Geotail MGF 16 vectors /sLEP 12 s
electron g-factor 4x10 T 5.5x10
-4
-3919:47
Tailward flows
Earthward flows
Bz < 0 Bz > 0
Tailward flows
Earthward flows
Ion Et
5 minutesBz > 0 Bz < 0
1019:47
Bz < 0 Bz > 0
Tailward flows
Earthward flows1000 km/s ion flow
VA = 2200 km/s
Bz > 0 Bz < 0
11
Ion observations
19:47
Bz < 0 Bz > 0
Vx > 3000 km/s electron flows
Vy > 6000 km/s electron flows
Ve
Vi
Ve
Bz > 0 Bz < 0
12
Ion flows vs. electron flows
Ion Et
19:47
Vx > 2000 km/s electron flows
Vy > 3000 km/s electron flows
VBz < 0 Bz > 0
Ve
Ve
Bz > 0 Bz < 0
Tailward flows
Earthward flows
13
Ion and electron flows
perpendicular to the magnetic field
19:47
Vx > 2000 km/s electron flows
Vy > 3000 km/s electron flows
VBz < 0 Bz > 0
Ve
Ve
Bz > 0 Bz < 0
14
Electron observations
acceleration and heating
electron Et
19:47
time
Bz > 0 Bz < 0
Tailward flowsEarthward flows
Bz > 0 Bz < 0
1057:44 1053:44 UT
15
> 8.47 keV electron directional fluxes
Earth tail
19:47
time
Bz > 0 Bz < 0
Tailward flowsEarthward flows
Bz > 0 Bz < 0
Vy < 0 dawnward
Vy > 0 duskward
electron velocitydistribution function
In the equatorial plane
1057:44 1053:44 UT
16
Earth tail
19:47
time
Bz > 0 Bz < 0
Tailward flowsEarthward flows
Bz > 0 Bz < 0
Hall electrons
electron velocitydistribution function
1057:44 1053:44 UT
17
Earth tail
19:47
time
Bz > 0 Bz < 0
Tailward flowsEarthward flows
Bz > 0 Bz < 0
ion velocitydistribution functions
1057:44 1053:44 UT
18
Earth tail
19:47
time
Bz > 0 Bz < 0
Tailward flowsEarthward flows
Bz > 0 Bz < 0
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1057:44 1053:44 UT
time
Bz > 0 Bz < 0
Tailward flowsEarthward flows
Bz > 0 Bz < 0
counter-streaming inflows
ion velocitydistribution functions
2019:47
1057:44 1053:44 UT
ion-electron decoupling Ve >> Vi
intense electron current layer
large Vey
spatial scales?
Important Questions
MHD MHD
1057:44 1053:44 UT
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+450 km/s -650 km/s
Earthward flow speed tailward flow speed
MHD flows
22
Asymmetric outflows
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+550 km/s -550 km/s(+450 km/s) (-650 km/s) -100 km/s
MHD flows
tailward velocity of reconnection site 2319:47
Vx = +64 km/s Vx= -269 km/s
inflows
24
Asymmetric inflows
19:47
Vx = +164 km/s Vx= -169 km/s (+264 km/s -269 km/s)
-100 km/s
inflows
Cluster results
-100 km/s Baker et al. 2002Imada et al. 2007
tailward velocity of reconnection site 2519:47
ion-electron decoupling region
8 i
central electron current layer
1 iMHD MHD
Vx peakFlux peak
Ion ele ele ion
Earth tail
8 i = 1.5 RE 1 i = 1200 km 2619:47
The simulation box size [−Lx/2,+Lx/2]×[−Lz/2,+Lz/2] Lx = 48D Lz = 24D
initial current sheet thickness D = 0.5λiΔ is equal to the Debye λi = 200Δ
The number of simulation grids 4800×2400
Particle number 1.5×10 particles for each species nCS Ti;CS/Te;CS = 5nBK = nCS Ti;BK = Te;BK = Te;CS
ion to electron mass ratio mi/me = 400
frequency ratio ωpe/Ωe = 4,ωpe ≡√4πnCSe2/me Ωe ≡ eB0/mec λi ≡ c/ωpi = c/√4πnCSe2/mi
The initial magnetic field the Harris sheet Bx(z) = B0 tanh(z/D) B0 the asymptotic magnetic field
D the current sheet half-thicknessThe perturbed magnetic flux function ψ(x, z) = ψ0 sin(2πx/Lx) cos(2πz/Lz)
B (x, z) = eˆy × ψ∇ (x, z)
at TΩi = 35 Vi x ∼ 0.3VA VA the Alfven speed B0/√4πminCS
9
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28
PIC simulation results
the northern earthward sideof the reconnection site(upper-left quadrant)
the X-line position
19:47
observation simulation at TΩi = 35
Vix / Vex 0.2-0.3 0.1
Vey / Vex 1.25 1.4
Vix 0.5 VA 0.3 VA
the full extent of the central 1 i 1 ielectron current layer
the full extent of 8 i 8 ithe ion-electron decouplingregion
2919:47
Geotail Survey ofTailward Flows with Bz < 0 in 1995-2003
209 events
Nagai et al., 2005 30
8 i = 1.5 RE ion-electron decoupling region
19:47
Geotail Reconnection Events= Observations of Ion-Electron Decoupling Region
34 events 34/208 = 0.16
reconnection events at 20-30 RE
Nagai et al., 1998; 20013119:47
Most of Events are MHD FlowsReconnection Events 34 events
34/208 = 0.16
reconnection events at 20-30 RE 10 RE x 0.16 = 1.6 RE
3219:478 i = 1.5 RE ion-electron decoupling region
ion-electron decoupling region
8 i
central electron current layer
1 iMHD MHD
Vx peakFlux peak
Ion ele ele ion
Earth tail
8 i = 1.5 Re 1 i = 1200 km 3319:47
Main conclusions
In the magnetic reconnection site of the near-Earth magnetotail
1.the central intense electron current layer 1 i2.ion-electron decoupling region 8 i3.MHD regions outside the i-e decoupling region
Nagai, T., I. Shinohara, M. Fujimoto, A. Matsuoka, T. Saito, and T. Mukai, J. Geophys. Res., 116, 2010JA016283, 2011.
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