Astrophysics of Planetary Systems Harvard 18 May 2004

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“Astrophysics of Planetary Systems” Harvard 18 May 2004 The Nature of Turbulence in Protoplanetary

“Astrophysics of Planetary Systems” Harvard 18 May 2004 The Nature of Turbulence in Protoplanetary Disks Jeremy Goodman Princeton University jeremy@astro. princeton. edu

Why do we care? • Spectrum depends on accretion rate only: – from boundary-layer

Why do we care? • Spectrum depends on accretion rate only: – from boundary-layer emission • Viscosity determines surface density: – not obviously compatible with viscosity • Agglomeration of solids (grains/planetesimals) • Gap formation & migration – & planetary eccentricities? • Unsteady behaviors – FU Orionis outbursts – Waves and wakes

Turbulence/Transport Mechanisms Candidate Pro Con Magnetorotational Instability (MRI) Robust linear instability. Well studied. ~10

Turbulence/Transport Mechanisms Candidate Pro Con Magnetorotational Instability (MRI) Robust linear instability. Well studied. ~10 -2 Uncertain nonthermal ionization required Finite-amplitude hydro instability Independent of ionization. Demonstrated in lab (? ) Poorly understood. Not confirmed by simulation Selfgravity Can be local. Reasonably well understood. Q>>1 in T Tauri phase Vertical convection Expected result of radiative Not driven by shear. cooling Transports J inwards. Radial convection / baroclinic instab. Ditto. Seems to make large Poorly understood. Linear instab. obscure vortices, ~10 -3 Planetary wakes Calculable. Inevitable at some level. Requires planets. Migration. <10 -4

MRI in Resistive Disks • MRI dynamo requires – Re. M 1 with imposed

MRI in Resistive Disks • MRI dynamo requires – Re. M 1 with imposed field • Ionization frac. crucial: – electron-neutral collisions • Thermal xe negligible @ T<1000 K • Nonthermal xe uncertain Fleming, Stone, & Hawley 2000 – Ionization rate: CR, Xrays, … – Recombination: dust, molecular ions, metal ions • Other wrinkles: – Layered accretion (Gammie ‘ 96) – Hall conductivity (Wardle ‘ 99) Fleming & Stone 2003

Resistive turbulence (Fleming et al. 2000)

Resistive turbulence (Fleming et al. 2000)

Further remarks on layered MRI • If CR=10 -17 s-1 & dissociative recomb. (after

Further remarks on layered MRI • If CR=10 -17 s-1 & dissociative recomb. (after Gammie ‘ 96) then in MMSN, – & accretion rate is too small:

Finite-amplitude hydro instability inner Richard & Zahn (1999): In MMSN: outer Richard 2001

Finite-amplitude hydro instability inner Richard & Zahn (1999): In MMSN: outer Richard 2001

 r -3/2 “Keplerian” profile found turbulent (Richard 2001)

r -3/2 “Keplerian” profile found turbulent (Richard 2001)

Objections to FAHI • Nonlocal: r not H is the lengthscale – H >

Objections to FAHI • Nonlocal: r not H is the lengthscale – H > r >> r in experiments – H << r ≈ r in accretion disks • Also compressible • No local linear instability for – But e. g. pipe flow is also linearly stable • Not found in local (shearing-sheet) simulations – But viscosity is explicitly nonlocal – Resolution or numerical Re may be inadequate • E. g. Longaretti 2002 • Doesn’t explain outbursts (e. g. dwarf novae)

Princeton MRI Experiment (H. Ji et al. ) B= 0. 7 T Re*~107 Re.

Princeton MRI Experiment (H. Ji et al. ) B= 0. 7 T Re*~107 Re. M ~ 1

Vortices & Baroclinic Instability • Anticyclonic vortices hold together by Coriolis force – Local

Vortices & Baroclinic Instability • Anticyclonic vortices hold together by Coriolis force – Local maximum in P & – Local minimum in vorticity: & vortensity: Godon & Livio 1999 • Realistically, • Wakes of persistent vortices transmit angular momentum Klahr & Bodenheimer 2003

Baroclinic Instability, continued • disks are typically unstably stratified in radius: – e. g.

Baroclinic Instability, continued • disks are typically unstably stratified in radius: – e. g. with dust opacity • Growth is nonaxisymmetric – Axisym’ly stable since – Linear growth is only transient due to shear (swing amplification) • Self-consistent ~10 -3 in 2 D & 3 D is claimed – Klahr & Bodenheimer 2003 • Confirmation is needed!

A plug for planetary wakes • A corotating obstacle---vortex or planet---has a wake –

A plug for planetary wakes • A corotating obstacle---vortex or planet---has a wake – Wavelike angular-momentum transport – Dissipation of gas orbits where wake shocks/damps • One planet: – Goodman & Rafikov ‘ 01; Rafikov ‘ 02 • Many planets: assuming – all metals in planets of equal mass Mp – planets distributed like gas Linearized wake in shearing sheet

Philosophical remarks • Turbulent “viscosity” probably depends on frequency – turb ~ , wake

Philosophical remarks • Turbulent “viscosity” probably depends on frequency – turb ~ , wake ~ ( r/H) turb • Angular momentum transport need not be turbulent – winds, wakes, … • Disks need not be smooth, even on lengthscales H & timescales -1 – Surely not on smaller scales! Nelson & Papaloizou ‘ 04

Peroration • MRI is the leading candidate but depends on uncertain microphysics and HE

Peroration • MRI is the leading candidate but depends on uncertain microphysics and HE irradiation – ISM theorists needed! • Finite-amplitude instability should be taken seriously – Higher-resolution simulations – Experiments with d(r 2 )/dr > 0 • Baroclinic instability needs to be confirmed – Simulations with independent codes • Investigate T( )