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Figure 1: The temporally and spatially averaged temperature structure of the 3D solar surface convection simulation (solid line) used for the 3D spectral line formation. The spatial averaging has been performed over surfaces of the same continuum optical depths at 500 nm. Note that the actual 3D simulation extends to much greater optical depths than shown here. Also shown are the temperature structures for the 1D Holweger-Müller (1974) semi-empirical solar atmosphere (dashed line) and the 1D MARCS (Asplund et al. 1997) theoretical solar atmosphere (dashed-dotted line). |
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Figure 2: Grotrian term-diagram of the employed 23-level O model atom with 22 bound states of O I and the ground state of O II. The forbidden [O I] 630.0 and 636.3 nm lines originate from the 2p4 3P ground state, while the O I 777 nm triplet is between the high-excitation 3s 5So and 3p 5P levels. The 43 bound-bound transitions are drawn. All O I levels are connected by bound-free transitions with the ground state of O II but are not shown for clarity. |
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Figure 3: The granulation pattern in one of the solar snapshots seen in disk-center continuum intensity at 777 nm ( upper left panel) and equivalent width of the O I 777.41 nm line in LTE ( upper right panel) and non-LTE ( lower left panel); the equivalent width images have the same relative intensity scale to emphasize the overall difference in line strengths. Also shown is the ratio of the non-LTE and LTE equivalent widths ( lower right panel). |
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Figure 4:
Predicted intensity ( |
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Figure 5:
Upper panel: the temporally and spatially averaged LTE flux profile
from the 3D model atmosphere (+) together with the observed profile (solid line)
for the O I 777.53 nm line. The theoretical profile has been computed with
log
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Figure 6:
The observed center-to-limb variations of the equivalent widths
of the O I 777 nm triplet are shown as
bands with estimated internal errors.
The solid lines denote the average
of two snapshots of the theoretical 3D non-LTE results for the three lines,
while the dashed lines represent the corresponding
3D LTE case. The here shown 3D LTE curves are very similar to the average of all 100
snapshots computed with the same 3D LTE line formation code used for
the calculations of the [O I] and OH lines. As two snapshots
are insufficient to yield an accurate abundance estimate, the 3D non-LTE results
have been interpolated to log
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Figure 7: The derived solar oxygen abundance (filled circles) from OH vibration-rotation lines using the 3D hydrodynamical time-dependent simulation of the solar atmosphere (Asplund et al. 2000b) as a function of wavelength, lower level excitation potential and line strength (in pm). The solid lines denote least-square-fits giving equal weights to all lines. |
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Figure 8:
Same as Fig. 7 but using the Holweger-Müller
(1974) semi-empirical model atmosphere and a microturbulence
of
|
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Figure 9:
Same as Fig. 7 but using
a theoretical MARCS model atmosphere (Asplund et al. 1997) and a microturbulence
of
|
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Figure 10: The derived solar oxygen abundance from OH pure rotational lines using a 3D hydrodynamical solar model atmosphere as a function of wavelength, lower level excitation potential and line strength (in pm). The solid lines denote the least-square-fits. The rotational lines are more sensitive to the adopted microturbulence than the vibration-rotation lines since the stronger lines are partly saturated. The increased scatter for the weakest lines (which correspond to the highest excitation lines) is most likely due to increased observational difficulties in measuring the equivalent widths accurately. |
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Figure 11:
Same as Fig. 10 but using the Holweger-Müller
model atmosphere. The filled circles correspond to
a microturbulence of
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Figure 12:
Same as Fig. 10 but using
a MARCS model atmosphere. The filled circles correspond to
a microturbulence of
|
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