研究目的
To measure the Rayleigh-scattering slope in the transmission spectrum of HD 189733b using the chromatic Rossiter-McLaughlin effect to show that it can be effectively used to measure broadband transmission features.
研究成果
Ground-based high-dispersion spectral observations can be used to probe broad-band features in the transmission spectra of extrasolar planets, such as the optical Rayleigh-scattering slope of HD 189733b, by using the chromatic Rossiter-McLaughlin effect. The precision achieved with HARPS per transit is about an order of magnitude lower than that with STIS on the Hubble Space Telescope. This method will be particularly interesting in conjunction with the new echelle spectrograph ESPRESSO, which currently is under construction for ESO’s Very Large Telescope, which will provide a gain in signal-to-noise ratio of about a factor 4 compared to HARPS.
研究不足
The precision achieved with HARPS per transit is about an order of magnitude lower than that with STIS on the Hubble Space Telescope. The method is affected by star spots and/or plages in a similar fashion as classical transmission spectroscopy.
1:Experimental Design and Method Selection:
The study used archival HARPS data of three transits of HD 189733b, covering a wavelength range of 400 to 700 nm. The radial velocity (RV) time-series were determined for white light and for six wavelength bins each 50 nm wide, using the cross-correlation profiles as provided by the HARPS data reduction pipeline. The RM effect was first fitted to the white-light RV time series using the publicly available code AROME.
2:Sample Selection and Data Sources:
The data were taken during the night of September 7, 2006, consisting of 28 exposures of 600 s each, and on the nights of July 19, 2007 and August 28, 2007, consisting of 38 and 40 exposures of 300 s each, respectively.
3:List of Experimental Equipment and Materials:
HARPS (High Accuracy Radial velocity Planet Searcher) spectrograph at the ESO
4:6 m telescope. Experimental Procedures and Operational Workflow:
The residuals to the best fit were subsequently subtracted from the RV time series of each wavelength bin, after which they were also fitted using the same code, leaving only the effective planet radius to vary.
5:Data Analysis Methods:
The chi-squared χ2 for each model to the data, with the uncertainties rescaled such that the reduced χ2 of the best-fit model is equal to unity. The 1σ-confidence interval was then determined by selecting the values of the radius ratio at which Δχ2 = 1.
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