Table 2:
Overview over the model parameters of the dynamical wind calculations.
is a parameter for the temperature dependence of the dust opacity (see Gail & Sedlmayr 1987).
![$M_\star [M_\odot]$](/articles/aa/full/2008/45/aa9243-07/img278.gif) |
: |
0.8, 1.0 |
![$L_\star [L_\odot]$](/articles/aa/full/2008/45/aa9243-07/img279.gif) |
: |
6000, 8000, 10 000 |
![$T_\star [{\rm K}]$](/articles/aa/full/2008/45/aa9243-07/img280.gif) |
: |
2400, 2600, 2800, 3000 |
![$\eta_{\rm opt} [{\rm K}^{-1}]$](/articles/aa/full/2008/45/aa9243-07/img281.gif) |
: |
4.4, 5.9 |
![$\sigma [{\rm K}]$](/articles/aa/full/2008/45/aa9243-07/img282.gif) |
: |
0, 20, 40, 60 |
![$[{\rm C/O}]$](/articles/aa/full/2008/45/aa9243-07/img283.gif) |
: |
1.8 |
![$P [{\rm days}]$](/articles/aa/full/2008/45/aa9243-07/img284.gif) |
: |
650 |
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