Sodium results Sample Clauses

Sodium results. The results for both methods of removal of the telluric water lines are shown, for the four passbands, in the second and third columns of Table 6.1. Both methods lines turn out to give similar results. The values agree in all four passbands with each other and with the literature values within their 1-σ uncertainties, with the exception of the values derived in the 4.4Å passband. The latter value derived using the second method lies just outside the uncertainties of the literature value and the value derived using the first method. The correction coefficient Passband [Å] This work Snellen et al. (2008) Sing et al. (2008a) Depth [%] 1.5 3.0 0.151±0.025 0.129±0.025 0.135±0.017 4.4 6.0 0.062±0.011 0.044±0.011 0.065±0.012 0.056±0.007 Table 6.1 — Comparison of the measurements of the sodium absorption by HD 209458b’s atmosphere for the two different methods of correcting for the telluric water lines. The first column shows the result for which the correction for telluric water lines was carried out in the transmission spectroscopy and the second column shows the results for which the telluric water lines have been removed in the spectra and only a small additional correction was carried out. The values are given together with their 1-σ uncertainties, as derived from the χ2 fit. The third and fourth columns show the results by Xxxxxxx et al. (2008) and Xxxx et al. (2008a). 0.055±0.015 0.053±0.015 0.070±0.011 0.052±0.010 0.042±0.010 used to scale the telluric spectrum and the coefficient used in the former method to remove the influence of telluric lines correlate linearly, which is also expected. Furthermore we measured, using the latter method, the relative line strength of the sodium absorption in two passbands around the two Na D lines varying in width from 0.75 Å, to 3 Å in steps of 0.035 Å. The transit curves are shown in Figure 6.7 for the passbands of 0.75 Å, 1.5 Å, and 3 Å chosen to be similar to those in Snellen et al. (2008). The left panels show the absorption in the D2 line, the middle panels in the D1 line, and the right panels show the average of the two. All these measurements are also given in Table 6.1, and compared with the Snellen et al. (2008) and Xxxx et al. (2008a) results. Instead of first conducting a fit only to the frames obtained outside of the transit, subse- quently measuring and removing the telluric line contribution, and finally measuring the ab- sorption depth, we also used the Xxxxxxxxx-Xxxxxxxxx least-squares minimization algor...
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