![\begin{figure}
\par\includegraphics[width=14.3cm,clip]{0089Fig1.epsf}\end{figure}](/articles/aa/full/2004/11/aa0089/Timg38.gif) |
Figure 1:
A schematic illustration of the jet-disk connection model. In the outer disk,
,
MFs are weak and advected around by fluid motion. Balbus-Hawley and
Parker-instabilities in combination with reconnection and fast
inwards fluid-motions amplify the MFs up to thermal equipartition
at
.
Interior to
,
MFs become of large scale
topology, strong, and start to suppress the generation of
turbulence, turning the inflow into a turbulent-free plasma. In
this case, torsional
waves become
the dominant angular momentum carrier. They transport angular momentum from
the disk upwards and form a super-Keplerian and dissipative layer, in which the plasma
is virial-heated by reconnection of the TMF, hence start to centrifugally-accelerate outwards.
Thus, the PMF in the equatorial layer is frozen into the plasma, and therefore is advected inwards
together with the inflow. The transition layers sandwiching the inner part of the disk
are dissipative. This allows the PMF to drift inwards through the plasma in the TL,
thereby relaxing the winding-up problem of the PMF. Thus, the
flow configuration may maintain stationarity, if the
plasma in the TLs is resistive, whereas it is diffusion-free in the disk. |