Bibcode
DOI
Emonet, T.; Moreno-Insertis, F.; Rast, M. P.
Bibliographical reference
The Astrophysical Journal, Volume 549, Issue 2, pp. 1212-1220.
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3
2001
Journal
Citations
15
Refereed citations
14
Description
We study the generation of vorticity in the magnetic boundary layer of
buoyant magnetic tubes and its consequences for the trajectory of
magnetic structures rising in the solar convection zone. When the
Reynolds number is well above 1, the wake trailing the tube sheds vortex
rolls, producing a von Kármán vortex street, similar to
the case of flows around rigid cylinders. The shedding of a vortex roll
causes an imbalance of vorticity in the tube. The ensuing vortex force
excites a transverse oscillation of the flux tube as a whole so that it
follows a zigzag upward path instead of rising along a straight vertical
line. In this paper, the physics of vorticity generation in the boundary
layer is discussed and scaling laws for the relevant terms are
presented. We then solve the two-dimensional magnetohydrodynamic
equations numerically, measure the vorticity production, and show the
formation of a vortex street and the consequent sinusoidal path of the
magnetic flux tube. For high values of the plasma beta, the trajectory
of the tubes is found to be independent of β but varying with the
Reynolds number. The Strouhal number, which measures the frequency of
vortex shedding, shows in our rising tubes only a weak dependence with
the Reynolds numbers, a result also obtained in the rigid-tube
laboratory experiments. In fact, the actual values measured in the
latter are also close to those of our numerical calculations. As the
Reynolds numbers are increased, the amplitude of the lift force grows
and the trajectory becomes increasingly complicated. It is shown how a
simple analytical equation (which includes buoyancy, drag, and vortex
forces) can satisfactorily reproduce the computed trajectories. The
different regimes of rise can be best understood in terms of a
dimensionless parameter, χ, which measures the importance of the
vortex force as compared with the buoyancy and drag forces. For
χ2<<1, the rise is drag dominated and the
trajectory is mainly vertical with a small lateral oscillation
superposed. When χ becomes larger than 1, there is a transition
toward a drag-free regime and epicycles are added to the trajectory.