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Figure 1:
Schematic representation of the free-standing vertical prominence slab. The slab has a geometrical extension L along the line-of-sight to the observer, at the altitude H above the limb. The prominence plasma is moving radially outwards at the velocity |
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Figure 2: Angle-averaged incident profiles in the prominence frame in the He I 584 line for a prominence located at 50 000 km above the limb, and for velocities ranging from 0 (solid line) to 240 km s-1 (step = 80 km s-1). The incident profile is shifted towards the red when the velocity increases. |
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Figure 3:
Differences between CRD (dashed line) and PRD (solid line) for the profiles of the three helium lines at different velocities: 0, 80, 160, and 240 km s-1 from top to bottom. Abscissa is
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Figure 4: Same as Fig. 3, with the abscissa now in Doppler units and limited to 10 Doppler widths around line centre, and the intensities on the vertical axis now shown on a log scale. The thin solid line shows the incident line profile, gradually shifting towards the red as the prominence is moving radially upwards. |
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Figure 5:
Comparison of the relative contribution of the Doppler core in the emitted line integrated intensities between CRD (dotted line) and PRD (solid line) calculations for He I
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Figure 6:
Comparison of the relative integrated intensities (integrated intensities normalised to the intensity at rest) between CRD (dotted line) and PRD (solid line) calculations for He I
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Figure 7:
Emergent intensities in erg s-1 cm-2 sr-1 as a function of radial velocity for He I
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Figure 8:
Relative intensity as a function of velocity at 8000 K (solid line) and 15 000 K (dotted line) for He I
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Figure 10:
Relative intensity as a function of velocity at 0.01 dyn cm-2 (dotted line) and 0.1 dyn cm-2 (solid line) for He I
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Figure 12: Population density of the ground level of He II as a function of velocity. The thickest lines refer to the mean population, the medium-thick line shows the level population at the surface of the slab, and the thinnest line corresponds to the population at slab centre. Solid lines: reference model with P=0.1 dyn cm-2; dashed lines: low-pressure model with P=0.01 dyn cm-2. |
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Figure 13:
Relative intensity as a function of velocity for a slab width of 200 km (dotted line) and 2000 km (solid line) for He I
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Figure 9:
Line profiles for T=8000 K (solid line) and T=15 000 K (dashed line), with p=0.1 dyn cm-2, and L=2000 km, at different velocities: 0, 40, 80, 120, 200 and 400 km s-1 from top to bottom. Abscissa is
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Figure 11: Line profiles for p=0.1 dyn cm-2 (solid line) and p=0.01 dyn cm-2 (dashed line), with T=8000 K and L=2000 km, at different velocities (same as in Fig. 9). |
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Figure 14: Line profiles for L=2000 km (solid line) and L=200 km (dashed line), with T=8000 K and p=0.1 dyn cm-2, at different velocities (same as in Fig. 9). |
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