Kinetic aspects of the vortex-induced
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Transcript Kinetic aspects of the vortex-induced
STP seminar, 14,July, 2010
Kinetic properties of magnetic reconnection
induced by the MHD-scale Kelvin-Helmholtz
vortex: particle simulations
中村 琢磨 (T.K.M. Nakamura)
Collaboraters:
H. Hasegawa, I. Shinohara, and M. Fujimoto
Plasma mixing of collisionless plasmas
In the MHD approximation, the frozen-in condition does
not allow for plasmas to mix across magnetic field lines.
BUT, for example, the Earth’s magentosphere contains
plasmas of solar wind origin.
⇒It means plasma mixing in fact occurs through the Earth’s
magnetopause.
Solving the plasma mixing mechanism in the Earth’s
magnetosphere leads to universal understanding of the
plasma mixing in space.
Dayside magnetic reconnection
The plasma mixing through the Earth’s magnetopause
occurs in any IMF (magnetic field of solar wind) conditions.
Especially when IMF is southward, the solar wind plasmas
can enter the magnetosphere relatively easily via dayside
magnetic reconnection.
[Dungey, 1961]
Earth’s Low-Latitude-Boundary-layer (LLBL)
Even when IMF is northward, the plasma mixing occurs
in the low-latitude boundary layer (LLBL).
[e.g., Mitchell et al., 1987; Hasegawa et al., 2003].
Kinetic properties of the LLBL
Particle velocity distribution functions shows the existence of bidirectional electrons in the mixing region of the LLBL.
[e.g., Hasegawa et al. , 2003; Fujimoto et al., 1998]
Hot magnetospheric ions
Cold magnetosheath ions
GEOTAIL
Bi-directional electrons
Bi
In the LLBL, mixed ions (and electrons) are observed accompanied with
bi-directionally accerelated electrons.
How to form the LLBL?
[Song & Russell, 1992]
[Hasegawa et al., 2004]
To explain how to form the LLBL under northward IMF, two major candidates have
been given,
1. double lobe reconnection at the high-latitude ⇒dayside LLBL?
2. Kelvin-Helmholtz vortices at the low-latitude. ⇒tail-flank LLBL?
BUT, the exact mixing mechanism by KH vortices has not yet been solved.
The KH vortex
2: magnetosheath
1: magnetosphere
The vortex-induced-reconnection by two-fluid simulation
[Nakamura et al., 2008]
Generally, a velocity boundary like the magnetopause is also a magnetic boundary.
⇒Past Linear analyses have shown that the Kelvin-Helmholtz vortex grows at the
magnetopause almost always accompanied with magnetic reconnection (that is,
the vortex-induced reconnection). [T.K.M. Nakamura et al., 2008]
The vortex-induced reconnection can lead to the plasma mixing along reconnected
field lines.
⇒The vortex-induced reconnection may form the LLBL.
To understand the exact mixing mechanism by the KH vortex,
we first performed kinetic simulations of the vortex-induced reconnection.
Initial conditions
method:2.5-dimensional full electromagnetic particle (EM-PIC) simulation [Nakamura et al., 2010]
-Initial parameters・N0=Ni0=const
・Bz0=4*B0 =const
・Bx0=B0*tanh(Y/D0) (current sheet)
・Vx0=V0*tanh(Y/D0) (velocity shear layer)
・D0=4.0, 2.0,1.0 [λi] (MHD-scale boundary layer)
・MA=V0/VA0=2.5(weak KHI)~5.0(strong KHI)
(KHI can grow when MA>2 [Miura & Pritchett, 1982] )
・Lx=λKH=20D0
(=fastest growing KH mode [Miura & Pritchett, 1982] )
・Ti/Te=1/8
・Mi/Me=25,100
・ωpe/Ωe=2.0
・100 particles/cell
Results
D0=2.0 (MHD-scale case),MA=4.375 (strong KHI case)
20li
In-plane magnetic field lines
Ion flow vectors
Y0
-20li
0
X
40li 0
X
40li
(T<50)The KHI grows and locally compresses the current sheet.
(T~50)Multiple reconnection occurs at the compressed thin current sheet.
(T~80)Finally, the KH vortex is highly rolled-up as a large magnetic island.
Multiple magnetic islands
In-plane magnetic field lines
20li
Y0
-20li
0
X
40li
(T=30-50)
The strong vortex flow produces a thin and long current.
(T=60-80)
Multiple magnetic islands are formed and move toward the main body of the
vortex.
(T~80)
Multiple magnetic islands are incorporated in turn into the vortex body via the
re-reconnection process.
Generality of the multiple islands formation
When Lcs>Lisland, more than one magnetic island can appear.
Since Lcs~5D0, and Lisland~12dmin,
the formation condition of magnetic islands is dmin/D0<0.4.
As D0, or MA decreases, dmin/D0 increases.
BUT, even in the smallest set of (D0,MA), dmin/D0<<0.4.
⇒The multiple islands formation can generally occur.
Generality of the multiple islands formation
(weak KHI)
(strong KHI)
Actually, in all cases, more than two magnetic islands appear.
The generation of multiple magnetic islands is a general feature
of the vortex-induced-reconnection.
Roles of RX in the vortex
Generally, reconnection can cause
1.the plasma mixing
2.the particle acceleration.
We investigated how the vortex-induced reconnection causes
the plasma mixing and particle acceleration processes.
ions
ele.
Roles of RX in the vortex
~plasma mixing~
(T~60-)
Both ions and electrons across the velocity
shear layer begin to mix from multiple X-lines.
(T~60-90)
The mixing area broadens along reconnected
field lines by the thermal speed.
(T=120)
Finally, inside of the vortex (island) becomes
filled with the well-mixed ions and electrons.
Plasma mixing rate of particles
initially existing at Y>0 and Y<0
The broadening for electrons is somewhat
faster than that for ions, since the thermal speed
for electrons is faster than that for ions.
Roles of RX in the vortex
~plasma mixing~
Mixing rate
1
ions
electrons
0
The mixing area broadens efficiently inside the
multiple magnetic islands.
Since the islands with well-mixed plasmas are
incorporated into the vortex body via re-RX,
the plasma mixing rapidly progresses while
the islands incorporation process continues.
(a) Total number of the mixed cells.
(b) Sketch of the plasma mixing process in
single X-line and multiple X-lines cases.
Roles of RX in the vortex
~electron acceleration~
Around the RX-points, the negative
reconnection electric field appears.
Around the re-RX points, the
positive reconnection electric field
appears.
Each reconnection electric field
intensity is almost consistent with the
reconnection rate at each
reconnection point (not shown).
Roles of RX in the vortex
~electron acceleration~
y
z
X
At RX-points, electrons are accelerated in the +Z-direction (almost same as the
parallel direction) by the negative reconnection electric field.
At re-RX points, electrons are accelerated in the -Z-direction (almost same as the
anti-parallel direction) by the positive reconnection electric field.
Roles of RX in the vortex
~electron acceleration~
Grid number normalized by the total grid number of
(red) the ion mixing area,(blue) electron mixing
area, (green) both ion and electron mixing area,
and (purple ) the area where plasma mixing and
bi-directional electrons coexist.
Since the re-RX process mixes electrons accelerated in the +Z and –Z directions,
inside of the vortex body is filled with the bi-directionally accelerated electrons.
⇒Mixed plasmas and bi-directional electrons inevitably
coexist inside the rolled-up vortex via a series of multiple
islands formation and incorporation processes.
Summary
Basic properties of the vortex-induced-reconnection
Multiple magnetic islands are generally formed at the
compressed thin current sheet by the vortex flow.
These islands are incorporated into the vortex body
via the re-reconnection process.
Kinetic roles of the vortex-induced-reconnection
The plasma mixing caused by the vortex-induced-reconnection is enhanced
by a series of multiple islands formation and incorporation processes.
Bi-directional accelerated electrons are produced inside the vortex
by a series of multiple islands formation and incorporation processes.
Thus, mixed plasma and bi-directional electrons (which are
the same features as the LLBL plasmas) inevitably coexist inside
the rolled-up vortex.
Observations of the vortex-induced-reconnection
Rolled-up vortices have successfully observed by Cluster [Hasegawa et al., 2004].
Observations of the vortex-induced-reconnection
Electron acceleration obsercved
aroud the vortex-induced RX region
[Hasegawa et al., 2009]
C1-C4 crossed a same current sheet between KH
vortices around 20:35:00UT.
C3 observed the evidence of reconnection.
C4 observed a bipolar BN fluctuation just after the CS
crossing!!
⇒This BN fluctuation could be the direct evidence of
the multiple islands formation process of the vortexinduced reconnection.
Observations of the island formation
THEMIS crossed the post-noon magnetopause.
Map of stream lines map from TH-A observations.
Moving magnetic islands (FTEs) were
commonly observed at the hyperbolic point of
the vortex flow.
[Eriksson et al., 2009]
Map of stream lines and field lines map from TH-A observations.
Roles of RX in the KH vortex
~mixing with bidirectional ele.~
What controls the thickness of the current sheet?
In ideal-MHD simulations, the current
sheet can become thinner at the
thickness of dx.
In particle simulations, before the
current sheet thickness reaches dx,
magnetic reconnection occurs.
⇒The lower limit of the current sheet
thickness is controlled by the vortexinduced-reconnection process.
What controls the thickness of the current sheet?
As the KHI grows, the current sheet
becomes thinner and thus the RX (tearing
instability) growth rate increases.
←The RX growth rate depends on the current
sheet thickness.
When the RX growth rate exceeds the KHI
growth rate (T~48), the linear growth of the
KHI finish and at the same time the current
sheet thinning begins to stop.
⇒The KHI growth rate controls
the minimum thickness of the
current sheet.
Roles of RX in the KH vortex
~electron acceleration~
Accelerated time period
Tacceleration ~ Le / Vinflow ~ le / Vinflow
Accelerated speed
Ve ~
e
e
E RX Tacceleration ~
Vinflow V Ai B0 le / Vinflow V Ae
me
me
Kinetic properties of the LLBL
Particle velocity distribution functions shows the existence of bidirectional electrons in the mixing region of the LLBL.
[e.g., Fujimoto et al., 1998]
electrons
ion
cold
anti-parallel
parallel
Hot
In the LLBL, mixed ions are observed with bi-directional electrons.
Dawn-dusk asymmetry of the LLBL
Particle velocity distribution functions shows a clear dawn-dusk
asymmetry in the mixing region of the LLBL .
dawnside
duskside
cold
Hot
The ion mixing regions are composed of
one-component ions.
(hot magnetospheric and cold
magnetosheath components not distinguished)
The ion mixing regions tend to be
composed of two-component ions.
⇒There is the large energy gap.
PIC simulations
We have performed 2.5D relativistic electromagnetic particle-in-cell (PIC) simulations
[Hoshino, 1987]. The basic equations we use are
1 E
B c0 J ,
c t
1 B
E,
c t
E
0
・・・Maxwell’s equations
B 0
, J
mj
d
1
V j q(E V j B),
2
dt
1 V / c
・・・Equation of motion for an ion and electron
where is the Lorentz factor, c is the speed of light and the suffix j is the particle number.
The charge density and the current density J is calculated by the PIC method.
Using initial density N0 and in-plane magnetic field B0, normalizations are made as follows:
the velocity, time, and length are normalized by the ion Alfven velocity VA B0 mi N 0 0
inverse of the ion gyrofrequency 1 mi eB0 , and the ion inertial length li VA i ,
respectively.
Earth’s Low-Latitude-Boundary-layer (LLBL)
density
temp.
The spacecraft ISEE-1 first detected the LLBL
[Sckopke et al, 1981].
The plasma mixing occurs inside the LLBL.
Dawn-dusk asymmetry of the LLBL
dawnside
duskside
[Hasegawa et al., 2003]
The ion mixing regions are formed
from one-component ions.
Under prolonged northward IMF,
the ion mixing regions tend to be
formed from two-component ions.