A three-dimensional Iroshnikov-Kraichnan phenomenology for MHD - - PowerPoint PPT Presentation

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A three-dimensional Iroshnikov-Kraichnan phenomenology for MHD - - PowerPoint PPT Presentation

A three-dimensional Iroshnikov-Kraichnan phenomenology for MHD turbulence in a strong mean magnetic field Wolf-Christian Mller Zentrum fr Astronomie und Astrophysik, TU Berlin Roland Grappin LUTH, Observatoire de Paris and LPP, Ecole


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SLIDE 1

A three-dimensional Iroshnikov-Kraichnan phenomenology for MHD turbulence in a strong mean magnetic field

Wolf-Christian Müller

Zentrum für Astronomie und Astrophysik, TU Berlin

Roland Grappin

LUTH, Observatoire de Paris and LPP, Ecole Polytechnique

Özgür Gürcan

LPP, Ecole Polytechnique

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SLIDE 2

Turbulence in Mean Magnetic Fields

Presumably different turbulent regimes → constraints on

  • timescales τ ac

, τ ac ⊥ (nonlinear time τNL = (k⊥b⊥)−1, Alfvén time τA = (kB0)−1)

  • Fourier space structure of turbulent excitations/driving

Established phenomenologies

◮ Strong regime (τNL ∼ τA): Goldreich-Sridhar (3D, k−5/3

), Boldyrev (3D, k−3/2

, ?)

◮ Weak regime (τNL ≫ τA, k⊥ ≫ k): e.g. Galtier, Ng & Bhattacharjee (3D, k−2

⊥ )

◮ Iroshnikov-Kraichnan (2D, k−3/2), weak turbulence variant, dwells only in 2D

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SLIDE 3

Universality

E3(k, θ) = A(θ)k−m−2 = A0(k/kd)−m−2, A(θ) ≃ kd(θ)m+2

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SLIDE 4

Fourier Energy Distribution (k-k⊥ plane)

Left: Critical balance cone (local frame): k ∼ k2/3

Middle: CB cone subject to fluctuations around mean direction ∼ b⊥

B0 ≃ 1 5

Right: DNS with isotropic large-scale driving Extent along k-axis apparently not explicable by reference-frame mapping

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SLIDE 5

A Different Regime of MHD turbulence

◮ No standard weak Alfvén turbulence (no nonlinear transfer in parallel direction) ◮ No standard critically balanced turbulence (geometrically too restricted) ◮ Suspected reason: isotropic large-scale driving ◮ Possibility of extension of IK picture to three-dimensionality

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SLIDE 6

General Nonlinear Triad Interaction

p q k Bo

Convolution constraint on three-mode interactions: k = p + q Example: finite q allows nonlinear field-parallel transfer

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SLIDE 7

Resonant Nonlinear Triad Interaction

p q k Bo

Convolution constraint on three-mode interactions: k = p + q Weak turbulence Resonance condition: ω(k) = ω(p) + ω(q) Alfvén waves: ω(k) = k · B0 = kB0 Resonance condition implies q = 0, i.e. no field-parallel cascade Phase-mixing along B0 prevents structure formation perpendicular to B0

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SLIDE 8

Causality

Generalization of GS-critical balance: τ ac

⊥ ∼ τ ac ∼ τA

Incompressible MHD (B0 2 − 3): τNL⊥ ∼ τA If transfer in planes perpendicular to B0 governed by IK cascade:

◮ τ ac

⊥ ∼ τA⊥ = (k⊥brms⊥)−1

◮ τA < τA⊥ < τNL

Relaxation of weak turbulence constraint (τA ≪ τNL) → possibility of quasi-resonant cascade, allows small q ∼ q⊥

brms⊥ B0

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SLIDE 9

Ricochet Process

Realizes energy flow along directions oblique w.r.t. B0

k_par k_per k1 k3 k5 k2 k4 k6 q1 q2 q3 q4 q5

Process based on two basic triads to transfer prolongations along two directions in Fourier space within region allowed by the quasi-resonance criterion. Dependent on dominant perpendicular cascade process populating excitations wi- thin the CB region. Start near Fourier origin requires externally excited fluctuations (e.g. isotropic large- scale forcing)

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SLIDE 10

Nonlinear Energy Flux

Isotropic K41 flux: FK41 ∼ kv3

k

(k−5/3) Iroshnikov-Kraichnan flux: FIK ∼ kb2

kb2 q/B0

(k−3/2) FIK approximately reduced by factor bq

B0

comparison with quasi-resonant flux (triad counting) Ensemble of triads reduced through quasi-resonance constraint by factor brms

B0

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SLIDE 11

Dissipative Regions

Estimating end of inertial range: τdiss ∼ τflux τ −1

diss ∼ νk2, τflux ∼ ku2

k

brms, τflux⊥ ∼ ku2

k

B0 (IK)

kd kd⊥ ∼ brms B0 Found in numerical simulations (Grappin & Müller 2010)

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Summary

◮ DNS of MHD turbulence with strong mean magnetic field, large-scale isotropic

driving incompatible with standard theory

◮ Proposition of new cascade mechanism based on weak IK cascade if turbulent

excitations outside critical balance region

◮ Ricochet mechanism allows for parallel and oblique nonlinear transport ◮ Three-dimensional extension of Iroshnikov-Kraichnan regime