Paradigm shifts in solar dynamo modeling
arXiv:0901.3789 · doi:10.1017/S1743921309030403
Abstract
Selected topics in solar dynamo theory are being highlighted. The possible relevance of the near-surface shear layer is discussed. The role of turbulent downward pumping is mentioned in connection with earlier concerns that a dynamo-generated magnetic field would be rapidly lost from the convection zone by magnetic buoyancy. It is argued that shear-mediated small-scale magnetic helicity fluxes are responsible for the success of some of the recent large-scale dynamo simulations. These fluxes help in disposing of excess small-scale magnetic helicity. This small-scale magnetic helicity, in turn, is generated in response to the production of an overall tilt in each Parker loop. Some preliminary calculations of this helicity flux are presented for a system with uniform shear. In the Sun the effects of magnetic helicity fluxes may be seen in coronal mass ejections shedding large amounts of magnetic helicity.
7 pages, 4 figures, final version
References in corpus (5)
- Global-Scale Turbulent Convection and Magnetic Dynamo Action in the Solar Envelope
- The case for a distributed solar dynamo shaped by near-surface shear
- Large-scale dynamos in turbulent convection with shear
- Turbulent magnetic Prandtl number and magnetic diffusivity quenching from simulations
- Nonlinear current helicity fluxes in turbulent dynamos and alpha quenching