Magnetic field generation on long time scales
description
Transcript of Magnetic field generation on long time scales
Magnetic field generation Magnetic field generation on long time scaleson long time scales
Axel Brandenburg (Nordita/Stockholm)
Kemel+12Kemel+12 Ilonidis+11Ilonidis+11 Brandenburg+11Brandenburg+11Warnecke+11Warnecke+11KKäpylääpylä+12+12
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White light image ofyesterday
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Tips of icebergs:Magnetic flux concentrations in magnetogram!
The thin flux tube paradigm
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Caligari et al. (1995) Charbonneau & Dikpati (1999)
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Standard dynamo waveStandard dynamo wave
Differential rotation(faster inside) Cyclonic convection;
Buoyant flux tubesEquatorward
migration
New loop
-effect
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Alternative proposal:Alternative proposal:Conveyor belt modelConveyor belt model
Dikpati et al. (2006)
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Simulations of the solar dynamo?Simulations of the solar dynamo?
• Tremendous stratification– Not only density, also scale height change
• Near-surface shear layer (NSSL) not resolved• Contours of cylindrical, not spoke-like• (i) Rm dependence (catastrophic quenching)
– Field is bi-helical: to confirm for solar wind
• (ii) Location: bottom of CZ or distributed– Shaped by NSSL (Brandenburg 2005, ApJ 625, 539)– Formation of active regions near surface
Brun, Brown, Browning, Miesch, ToomreBrun, Brown, Browning, Miesch, Toomre
8Brown et al. (2011)ASH code: anelastic
spherical harmonics
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• Cycle now common!
• Activity from bottom of CZ
• but at high latitudes
Ghizaru, Ghizaru, Charbonneau, Charbonneau,
Racine, …Racine, …
Racine et al. (2011)
PencilPencilcodecode
• Started in Sept. 2001 with Wolfgang Dobler• High order (6th order in space, 3rd order in time)• Cache & memory efficient• MPI, can run PacxMPI (across countries!)• Maintained/developed by ~80 people (SVN)• Automatic validation (over night or any time)• 0.0013 s/pt/step at 10243 , 2048 procs• http://pencil-code.googlecode.com
• Isotropic turbulence– MHD, passive scl, CR
• Stratified layers– Convection, radiation
• Shearing box– MRI, dust, interstellar– Self-gravity
• Sphere embedded in box– Fully convective stars– geodynamo
• Other applications– Chemistry, combustion– Spherical coordinates
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Dynamo wave from simulations Kap
yla et al (2012)
Type of Type of dynamo?dynamo?
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• Use phase relation
• Closer to 2 dynamo
• Wrong for dyn.
Mitra et al. (2010)
Oscillatory 2 dynamo
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Remaining aspectsRemaining aspects
(i) Bi-helical fields inverse cascade
(ii) Solar wind also bi-helical field
(iii) Formation of active regions at solar surface
(i) Dynamo produces bi-helical field(i) Dynamo produces bi-helical field
BAdkkH )(
Magnetic helicity spectrum
031 / bjuω
Pouquet, Frisch, & Leorat (1976)
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Helicity fluxes to alleviate Helicity fluxes to alleviate catastrophic quenchingcatastrophic quenching
Bra
nden
burg
(20
05, A
pJ)
1046 Mx2/cycle
FBJBA 2d
d
t
Magnetic helicity fluxMagnetic helicity flux
• EMF and resistive terms still dominant
• Fluxes import at large Rm ~ 1000
• Rm based on kf
• Smaller by 2
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m22d
dF BJBBA ε
t
f22d
dF bjBba ε
t
Magnetic helicity fluxMagnetic helicity flux
• EMF and resistive terms still dominant
• Fluxes import at large Rm ~ 1000
• Rm based on kf
• Smaller by 2
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m22d
dF BJBBA ε
t
f22d
dF bjBba ε
t
Gauge-invariant in steady state!
Del Sordo, Guerrero, Brandenburg (2013, MNRAS 429, 1686)
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This is how it looks like…This is how it looks like…Coronal mass ejections from helical structures
Gibson et al. (2002)
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(ii) Helicity from solar wind(ii) Helicity from solar wind
)()( xBxBM jiij
)(
)()(
kHki
kEkkkM
kijk
jiijij
)()( xBxBM jiij
)()()( rxxr jiij BBM
Matthaeus et al. (1982) Measure correlation function
In Fourier space, calculatemagnetic energy and helicity spectra
Should be done with Ulysses data away from equatorial plane
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Measuring 1-D correlation tensorMeasuring 1-D correlation tensor
tuRR R 0Taylor hypothesis:
RRNRTR kkBkBkH /)()(~
Im4)( *
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Bi-helical fields from UlyssesBi-helical fields from Ulysses
• Taylor hypothesis• Broad k bins• Southern latitude
with opposite sign• Small/large distances• Positive H at large k• Break point with
distance to larger k
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ComparisonComparison
• Field in solar wind is clearly bi-helical
• ...but not as naively expected
• Need to compare with direct and mean-field simulations
• Recap of dynamo bi-helical fields
Helicity LS SS
Dynamo + -
Solar wind - +
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Dynamos with exterior Dynamos with exterior CMEs? CMEs?W
arnecke, B
randen
burg, Mitra (2011, A
&A
, 534, A11)
24Strong fluctuations, but positive in north
War
nec
ke, B
rand
enbu
rg, M
itra
(20
11, A
&A
, in
pre
ss)
Shell dynamos with ~CMEsShell dynamos with ~CMEs
To carry negative flux: need positive gradientTo carry negative flux: need positive gradient
f2f
m2m
22d
d
22d
d
FBJB
FBJB
t
t
t
h
t
h
Brandenburg, Candelaresi, Chatterjee(2009, MNRAS 398, 1414)
Sign reversal makes sense!
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(iii) How deep are sunspots rooted?(iii) How deep are sunspots rooted?
• Solar activity may not be so deeply rooted• The dynamo may be a distributed one• Near-surface shear important
Hindm
an et al. (2009, ApJ)
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Two alternative sunspot originsTwo alternative sunspot origins
Theories for shallow spots:Theories for shallow spots:
(i) Collapse by suppression(i) Collapse by suppressionof turbulent heat fluxof turbulent heat flux
(ii) Negative pressure effects(ii) Negative pressure effectsfrom <from <uuiiuujj> vs > vs BBiiBBjj
Kosovichev et al. (2000)
Kosovichev et al. (2000)
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Negative effective magnetic pressure instability
• Gas+turb. press equil.
• B increases
• Turb. press. Decreases
• Net effect?
Self-assembly of a magnetic spot• Minimalistic model• 2 ingredients:
– Stratification & turbulence
• Extensions– Coupled to dynamo– Compete with rotation– Radiation/ionization
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Imposed vs. self-assembly• Appearance of sunspot
when coupled to radiation
• Can be result of self-assembly when ~1000 G field below surface
30Stein & Nordlund (2012)
Rempel et al. (2009)
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ConclusionsConclusions• Interest in predicting solar activity
• Cyclonic convection ( helicity)
• Near surface shear migratory dynamo
• Bi-helical fields, inverse cascade
• Solar wind also bi-helical field, but reversed
• Formation of active regions and sunspots by negative effective magnetic pressure inst.