A SYSTEMATIC RETRIEVAL ANALYSIS OF SECONDARY ECLIPSE SPECTRA. I. A COMPARISON OF ATMOSPHERIC RETRIEVAL TECHNIQUES

被引:294
作者
Line, Michael R. [1 ]
Wolf, Aaron S. [1 ]
Zhang, Xi [1 ]
Knutson, Heather [1 ]
Kammer, Joshua A. [1 ]
Ellison, Elias [2 ]
Deroo, Pieter [3 ]
Crisp, Dave [3 ]
Yung, Yuk L. [1 ]
机构
[1] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
[2] Flintridge Preparatory Sch, La Canada Flintridge, CA 91011 USA
[3] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
基金
美国国家航空航天局;
关键词
methods: data analysis; methods: statistical; planets and satellites: atmospheres; radiative transfer; COLLISION-INDUCED ABSORPTION; THERMAL EMISSION; TRANSMISSION SPECTROSCOPY; HD; 209458B; DAYSIDE SPECTRUM; HOT JUPITERS; H-2; PAIRS; TEMPERATURE; PLANETS; WATER;
D O I
10.1088/0004-637X/775/2/137
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Exoplanet atmosphere spectroscopy enables us to improve our understanding of exoplanets just as remote sensing in our own solar system has increased our understanding of the solar system bodies. The challenge is to quantitatively determine the range of temperatures and molecular abundances allowed by the data, which is often difficult given the low information content of most exoplanet spectra that commonly leads to degeneracies in the interpretation. A variety of spectral retrieval approaches have been applied to exoplanet spectra, but no previous investigations have sought to compare these approaches. We compare three different retrieval methods: optimal estimation, differential evolution Markov chain Monte Carlo, and bootstrap Monte Carlo on a synthetic water-dominated hot Jupiter. We discuss expectations of uncertainties in abundances and temperatures given current and potential future observations. In general, we find that the three approaches agree for high spectral resolution, high signal-to-noise data expected to come from potential future spaceborne missions, but disagree for low-resolution, low signal-to-noise spectra representative of current observations. We also compare the results from a parameterized temperature profile versus a full classical Level-by-Level approach and discriminate in which situations each of these approaches is applicable. Furthermore, we discuss the implications of our models for the inferred C-to-O ratios of exoplanetary atmospheres. Specifically, we show that in the observational limit of a few photometric points, the retrieved C/O is biased toward values near solar and near one simply due to the assumption of uninformative priors.
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页数:22
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