This page is a short introduction to the hybrid interface dynamo mode. This bybrid dynamo mode covers all latitudes because the toroidal field regeneration occurs through the agency of the positive latitudinal shear, which exists at all latitudes above and below the core-envelope interface. This is a hybrid mode, in the sense that in requires the presence of a shear both above and below the interface. An animation and butterfly diagrams can be viewed by clicking on their respective iconic images below.
On the animation, the dynamo mode
is displayed in a full meridional plane (left), with the rotation
axis located along the right edge of the panel. The solution is
also displayed in a cartesian closeup about the core-envelope
interface (right), with the polar axis corresponding to the left
edge of the panel, the equatorial plane to the right edge, and
the core-envelope interface running horizontally through the middle
of the panel. Note that vertically, this closeup covers only
10% of the solar radius.
The color scale codes the magnitude of the toroidal
component of the magnetic field: yellow-orange-red is positive,
green-cyan-blue negative, each covering 5 orders of magnitude
in field strength. The poloidal magnetic component
is shown as fieldlines (white/gray=clockwise/counterclockwise
orientation).
Click here to view animation [Size: 642 KB]
Butterfly diagrams are constant-radius cuts showing the latitudinal
distribution (vertical) of the magnetic field evolving in time
(horizontal). The bottom panel is a butterfly diagram for the
toroidal field within the shear layer (color coding as on animation).
The top panel is a butterfly diagram for the radial component of
the poloidal field at the solar surface.
Click here to view butterfly diagram
Copyright 1996, NCAR.
Last revised June 28, 1996 - P. Charbonneau