Spontaneous formation of flux concentrations in a stratified layer
arXiv:1112.0279 · doi:10.1007/s11207-012-9949-0
Abstract
The negative effective magnetic pressure instability discovered recently in direct numerical simulations (DNS) may play a crucial role in the formation of sunspots and active regions in the Sun and stars. This instability is caused by a negative contribution of turbulence to the effective mean Lorentz force (the sum of turbulent and non-turbulent contributions) and results in formation of large-scale inhomogeneous magnetic structures from initial uniform magnetic field. Earlier investigations of this instability in DNS of stably stratified, externally forced, isothermal hydromagnetic turbulence in the regime of large plasma beta are now extended into the regime of larger scale separation ratios where the number of turbulent eddies in the computational domain is about 30. Strong spontaneous formation of large-scale magnetic structures is seen even without performing any spatial averaging. These structures encompass many turbulent eddies. The characteristic time of the instability is comparable to the turbulent diffusion time, L^2/eta_t, where eta_t is the turbulent diffusivity and L is the scale of the domain. DNS are used to confirm that the effective magnetic pressure does indeed become negative for magnetic field strengths below the equipartition field. The dependence of the effective magnetic pressure on the field strength is characterized by fit parameters that seem to show convergence for larger values of the magnetic Reynolds number.
14 pages, 8 figures, submitted to special issue "Advances of European Solar Physics" in Solar Physics
References in corpus (11)
- The case for a distributed solar dynamo shaped by near-surface shear
- Simulation of the Formation of a Solar Active Region
- Penumbral structure and outflows in simulated sunspots
- Penumbral fine structure and driving mechanisms of large-scale flows in simulated sunspots
- Kinematic alpha effect in isotropic turbulence simulations
- Magnetic fluctuations and formation of large-scale inhomogeneous magnetic structures in a turbulent convection
- Subsurface magnetic field and flow structure of simulated sunspots
- Detection of negative effective magnetic pressure instability in turbulence simulations
- Dynamo action and magnetic buoyancy in convection simulations with vertical shear
- Properties of the negative effective magnetic pressure instability
- Pumping velocity in homogeneous helical turbulence with shear
Cited by in corpus (21)
- Current status of turbulent dynamo theory: From large-scale to small-scale dynamos
- Astrophysical hydromagnetic turbulence
- Advances in mean-field dynamo theory and applications to astrophysical turbulence
- Negative effective magnetic pressure in turbulent convection
- Active region formation through the negative effective magnetic pressure instability
- Self-assembly of shallow magnetic spots through strongly stratified turbulence
- Mean-field and direct numerical simulations of magnetic flux concentrations from vertical field
- Intense bipolar structures from stratified helical dynamos
- Magnetic flux concentrations from turbulent stratified convection
- Magnetic concentrations in stratified turbulence: the negative effective magnetic pressure instability
- Magnetic flux concentrations from dynamo-generated fields
- Bipolar region formation in stratified two-layer turbulence
- Rotational effects on the negative magnetic pressure instability
- Surface flux concentrations and spherical alpha-square dynamo
- Magnetic flux concentrations in a polytropic atmosphere
- Nonlinear mean-field dynamo and prediction of solar activity
- The turbulent pressure of magnetoconvection for slow and rapid rotation
- A new look at sunspot formation using theory and observations
- Nonuniformity effects in the negative effective magnetic pressure instability
- Magnetic bipoles in rotating turbulence with coronal envelope
- Non-linear and chaotic dynamo regimes