Solar activity as a surface phenomenon

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Solar activity as a surface Solar activity as a surface phenomenon phenomenon Axel Brandenburg (Nordita/Stockholm) Kemel+12 Kemel+12 Ilonidis+11 Ilonidis+11 Brandenburg+ Brandenburg+ 11 11 Warnecke+11 Warnecke+11 K äpylä äpylä +12 +12

description

Solar activity as a surface phenomenon. Axel Brandenburg (Nordita/Stockholm). Kemel+12. K äpylä +12. Ilonidis+11. Warnecke+11. Brandenburg+11. The thin flux tube paradigm. Caligari et al. (1995). Charbonneau & Dikpati (1999). Spruit paper. Standard dynamo wave. New loop. - PowerPoint PPT Presentation

Transcript of Solar activity as a surface phenomenon

Page 1: Solar activity as a surface phenomenon

Solar activity as a surface Solar activity as a surface phenomenonphenomenon

Axel Brandenburg (Nordita/Stockholm)

Kemel+12Kemel+12 Ilonidis+11Ilonidis+11 Brandenburg+11Brandenburg+11Warnecke+11Warnecke+11KKäpylääpylä+12+12

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The thin flux tube paradigm

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Caligari et al. (1995) Charbonneau & Dikpati (1999)

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Spruit paper

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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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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

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Brun, Brown, Browning, Miesch, ToomreBrun, Brown, Browning, Miesch, Toomre

6Brown 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)

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Dynamo wave from simulations Kap

yla et al (2012)

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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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Turbulent sunspot origins?Turbulent 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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Turbulent sunspot origins?Turbulent sunspot origins?

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Negative effective magnetic pressure instability

• Gas+turb. press equil.

• B increases

• Turb. press. Decreases

• Net effect?

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Much stronger with vertical fields

• Gas+turb. press equil.

• B increases

• Turb. press. Decreases

• Net effect?

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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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Sunspot decay

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5123 vs 10243 resolution

• Rm/Re dependence?

• Here 40/80 and 95/190

• Originally 18/36.

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Surface-filling magnetic activity

17Guedel (2004)Saturated activity naturally explained

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3 times stronger stratification

• Rm/Re dependence?

• Here 40/80 and 95/190

• Originally 18/36.

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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

19Stein & Nordlund (2012)

Rempel et al. (2009)

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Why so strong?

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Vertical fields survive downward flow

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ConclusionsConclusions• Interest in predicting solar activity

• Cyclonic convection ( helicity)

• Near surface shear migratory dynamo?

• Formation of active regions and sunspots by negative effective magnetic pressure inst.