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Figure 1: Observational data used for this paper. The wavelength coverage of the different instruments is shown. |
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Figure 2:
The contribution of different molecules to
the formation of the synthetic spectrum of in
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Figure 3: Partition functions of molecules H2O and HDO. Our data for H2O are compared with Vidler & Tennyson (2000), data for HDO are compared with Hewitt et al. (2005). Our partition function for HDO is computed for s1 =1. The differences in the HDO partition functions at higher temperatures (T > 4000 K) are due to the use of more complete sets of deuterated water levels in the UCL model compared with the AMES model. |
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Figure 4: Molecular densities of H2O computed for NextGen model atmospheres 2800/5.0 and 3800/5.0 for the cases of partition functions computed with si = 1, 4 and si =1/4, 3/4. |
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Figure 5: Responses of computed spectra to variations of input parameters. A model atmosphere of 3000/5.0/0.0 was used as the reference model. |
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Figure 6: Top: temperature structure of model NextGen, DUSTY and COND model atmospheres of 2800/5.0/0. Bottom: ratio of fluxes computed for these model atmospheres. |
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Figure 7: Ratio of fluxes computed for 2800/5.0 NextGen model atmosphere with TiO line lists by Plez (1998) and Schwenke (1998). |
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Figure 8:
Min
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Figure 9: Fits with linear and logarithmic flux scales to our GJ406 spectrum with a theoretical spectrum computed for a solar composition NextGen model atmosphere 2800/5.0. |
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Figure 10:
A comparison of
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Figure 11:
Top: location of GJ 406
in respect to
the Baraffe et al. (1998) evolutionary tracks and
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