Grand minima in a buoyancy-driven solar dynamo

Astronomy and Astrophysics – Astrophysics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

15

Sun: Magnetic Fields, Sun: Activity, Magnetic Fields, Magnetohydrodynamics (Mhd)

Scientific paper

Numerical simulations of a 2D mean-field model are presented which show that grand minima, typical for the long-term behaviour of solar magnetic activity, can be produced by a dynamo that features an alpha effect based on the buoyancy instability of magnetic fluxtubes. The buoyancy-driven alpha effect functions only if the magnetic field strength exceeds a minimal value necessary for instability. It opens the possibility of dynamo action within the solar overshoot layer, where a strong magnetic field, B~ 105 G, is thought to be stored. The existence of a magnetic threshold for dynamo action can lead to interruptions of the magnetic cycle, similar to the grand minima of solar activity. Transitions across the instability threshold are triggered by magnetic-flux injections from the convection zone. This is modelled by allowing for a small-scale kinematic alpha effect in the convection zone, and convective downdrafts that penetrate the overshoot layer.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Grand minima in a buoyancy-driven solar dynamo does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Grand minima in a buoyancy-driven solar dynamo, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Grand minima in a buoyancy-driven solar dynamo will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1717146

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.