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Figure 1: Radius is plotted over optical depth. The optical depth was calculated from the wavelength independent continuous opacity. The atmosphere is about 60 m thick, but the layers with an optical depth around one lie just centimeters below the outermost layer. |
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Figure 2: Results for non-scattering model line and continuum. |
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Figure 3:
The model line and the continuum are scattering with
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Figure 4:
The model line scatters with
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Figure 5:
The model line is nonscattering with a completely scattering -
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Figure 6:
The model line is completely scattering -
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Figure 7:
The spectrum was corrected for the gravitational redshift and fitted
with a blackbody with the known effective temperature of the model -
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Figure 8:
The spectrum was corrected for the gravitational redshift and fitted
with a blackbody with the known effective temperature of the model -
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Figure 9: The model spectrum is the same as in Fig. 8, but this time the temperature of the blackbody was chosen to fit the spectrum. |
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Figure 10:
The spectrum was corrected for the gravitational redshift and fitted
with a blackbody with the known effective temperature of the model -
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Figure 11: The model spectrum is the same as in Fig. 10, but this time the temperature of the blackbody was chosen to fit the spectrum. |
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Figure 12: Thermalisation depth is plotted over optical depth. Since the radial structure is only known on a discrete grid the value of the thermalisation depth for a given temperature was determined via linear interpolation. |
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