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This research attempts to better understand the process
of solar magnetic field generation by investigating the origin of
strong magnetic fields that emerge at the solar surface. This field
is believed to be derived from a strong toroidal magnetic field
generated in a layer just below the base of the solar convection
zone, called the tachocline. The tachocline is a thin region of
stability located below the unstably stratified convection zone.
A thin horizontal magnetic field is arbitrarily introduced into
the upper layer of a simulated solar convection zone. To maintain
constant pressure, the density of the fluid inside the magnetic
field is reduced. Hence the magnetic field is buoyant relative to
its surroundings. In the absence of convective motion the magnetic
field would rise. However, the highly turbulent convection zone
drags components of the magnetic field down into the stably stratified
layer by the advection of downward flowing plumes. As these plumes
penetrate the stable layer in an area called the "overshoot"
region, they decelerate rapidly. This rapid deceleration causes
the plumes to "splash" and produce numerous small vortices.
These highly turbulent vortices stretch the magnetic field and amplify
its strength through local dynamo action. The net effect is a redistribution
of magnetic energy as the magnetic field is both pumped into the
tachocline region and then amplified. |
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Pumping Magnetic Fields

QuickTime
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In the left cube is the enstrophy
(rotation) component of a solar convection zone. On the right, a
magnetic bouncy field is depicted. The magnetic field has been arbitrarily
introduced into the convection zone.Ê
Observe a downward flowing plume in the lower, left corner
of the enstrophy domain. As we evolve through time, the magnetic
field tries to rise due to bouncy. However, the competing effects
of convective motion drag components of the field into the lower
half of the domain. |
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Down-plume Zoom

QuickTime
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Zooming in on the down-plume, we see
how it interacts with the magnetic field. Notice how the field gets
stronger (brighter colors) in the lower domain as the field is amplified
by local dynamo action. |
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| Visualization |
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Visualization: |
John Clyne, NCAR, SCD
Nic Brummell, University of Colorado |
| Project |
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Scientists: |
Steve Tobias, University of Colorado
Nic Brummell, University of Colorado
Tom Clune, University of Colorado
Juri Toomre, University of Colorado |
Date Catalogued: |
2002-08-12 |
Rights: |
© 2002, UCAR,
All rights reserved. |
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