J/ApJ/774/6    Empirical scaling laws for shell dynamos       (Yadav+, 2013)

Consistent scaling laws in anelastic spherical shell dynamos. Yadav R.K., Gastine T., Christensen U.R., Duarte L.D.V. <Astrophys. J., 774, 6 (2013)> =2013ApJ...774....6Y 2013ApJ...774....6Y
ADC_Keywords: Models ; Magnetic fields Keywords: brown dwarfs; convection; methods: numerical; stars: interiors; stars: low-mass; stars: magnetic field Abstract: Numerical dynamo models always employ parameter values that differ by orders of magnitude from the values expected in natural objects. However, such models have been successful in qualitatively reproducing properties of planetary and stellar dynamos. This qualitative agreement fuels the idea that both numerical models and astrophysical objects may operate in the same asymptotic regime of dynamics. This can be tested by exploring the scaling behavior of the models. For convection-driven incompressible spherical shell dynamos with constant material properties, scaling laws had been established previously that relate flow velocity and magnetic field strength to the available power. Here we analyze 273 direct numerical simulations using the anelastic approximation, involving also cases with radius-dependent magnetic, thermal, and viscous diffusivities. These better represent conditions in gas giant planets and low-mass stars compared to Boussinesq models. Our study provides strong support for the hypothesis that both mean velocity and mean magnetic field strength scale as a function of the power generated by buoyancy forces in the same way for a wide range of conditions. File Summary: -------------------------------------------------------------------------------- FileName Lrecl Records Explanations -------------------------------------------------------------------------------- ReadMe 80 . This file table1.dat 89 11 Simulation setups table2.dat 130 273 Simulation dataset used in the article to infer various scaling laws -------------------------------------------------------------------------------- Byte-by-byte Description of file: table1.dat -------------------------------------------------------------------------------- Bytes Format Units Label Explanations -------------------------------------------------------------------------------- 1- 3 A3 --- SID Subset name (A=Anelastic; B=Boussinesq) 5- 6 I2 --- N [1/58] Number of cases 8- 17 A10 --- Core Core description ("Insulating" or "Conducting") 19- 23 A5 --- BC Mechanical boundary condition (1) 25- 28 F4.2 --- eta [0.1/0.8] Aspect ratio η (inner radius to outer radius ratio of shell with dynamo action) 30- 35 A6 --- g(r) Gravity profile g(r) (2) 37- 39 F3.1 --- m [0/2] Polytropic index m (2) 41- 46 A6 --- Pr Prandtl number Pr range 48- 53 A6 --- Pm Magnetic Prandtl number Pm range (ratio of viscosity ν and thermal diffusivity κ) 55- 58 E4.1 --- E Ekman number E (or lower range) 59 A1 --- --- [-] 60- 63 E4.1 --- E2 ? Ekman number (upper range) 65- 70 A6 --- Nrho Number of density scale heights inside the shell Nρ 72- 89 A18 --- Var Varying inside the shell (3) -------------------------------------------------------------------------------- Note (1): Mechanical boundary conditions are: SF = shear stress free on both boundaries Mixed = rigid inner and stress-free outer boundary Note (2): Gravity profile as in equation (1): g(r)=g1(r/r0)+g2(r20/r2) and by using g1 or g2 appropriately we can either choose a linear gravity profile (g1=1, g2=0), approximately representing a self-gravitating body with weak density variation, or an r-2 gravity profile (g1=0, g2=1), exemplifying objects with a massive core. Assuming an ideal gas equation of state leads to a polytropic reference state defined by ρ=Tm, where m is the polytropic index. See section 2.1. Note (3): Transport properties which vary along the shell radius, where ν is the kinematic viscosity, κ the thermal diffusivity and λ the magnetic diffusivity. In groups A2b and B1b the variation of λ is obtained from Equation (11) and in group A4 the variation follows Equation (12). -------------------------------------------------------------------------------- Byte-by-byte Description of file: table2.dat -------------------------------------------------------------------------------- Bytes Format Units Label Explanations -------------------------------------------------------------------------------- 1- 3 A3 --- SID Simulation identifier (as in table 1) 5- 12 E8.2 --- E Ekman number E=ν/(ΩD2) 14- 17 F4.1 --- Pr [0/10] Prandtl number Pr=ν/κ 19- 22 F4.1 --- Pm [0/20] Magnetic Prandtl number Pm=ν/λ 24- 31 E8.2 --- Ra Rayleigh number Ra 33- 36 F4.2 --- Nrho [0/5.5] Number of density scale heights Nρ 38- 46 F9.5 --- Mass [8/630] Non-dimensional mass of spherical shell 48- 51 F4.2 --- chim [0.7/1]? Fraction of total radius (1) 53- 63 E11.5 --- P [2.e-8/3.e-2] Non-dimensional buoyancy power (2) 65- 74 F10.8 --- Ro [0.001/0.44] Rossby number defined by Eq.13 76- 85 F10.8 --- Roconv [0.001/0.3] Rossby number (3) 87- 97 F11.9 --- Lo [0/0.1] Lorentz number defined by Eq.14 99-107 F9.7 --- fohm [0/0.7] Ohmic fraction defined by Eq.17 109-118 F10.6 --- taumag [0.7/135] Magnetic dissipation time τmag defined by Eq.18 120-130 E11.5 --- fdip Dipolarity (4) -------------------------------------------------------------------------------- Note (1): After which exponential decay of electrical conductivity starts. Blanks indicated Not Applicable. Note (2): Per unit mass defined by Eq.15. Note (3): Defined by excluding zonal and meridional flow components. Note (4): The dipolarity fdip is the magnetic energy in the axisymmetric dipole normalized by the cumulated magnetic energy in harmonic degrees up to 12, both evaluated at the outer boundary. Dynamos with fdip>0.3 are considered dipolar. See section 3.1. -------------------------------------------------------------------------------- History: From electronic version of the journal
(End) Greg Schwarz [AAS], Emmanuelle Perret [CDS] 25-Feb-2015
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