Detectability of biosignatures on LHS 1140 b

被引:24
作者
Wunderlich, Fabian [1 ,2 ]
Scheucher, Markus [1 ,2 ]
Grenfell, John Lee [2 ]
Schreier, Franz [3 ]
Sousa-Silva, Clara [4 ]
Godolt, Mareike [2 ]
Rauer, Heike [1 ,2 ,5 ]
机构
[1] Tech Univ Berlin, Zentrum Astron & Astrophys, Hardenbergstr 36, D-10623 Berlin, Germany
[2] Inst Planeten Forsch, Deutsch Zentrum Luft & Raumfahrt, Rutherfordstr 2, D-12489 Berlin, Germany
[3] Deutsch Zentrum Luft & Raumfahrt, Inst Method Fernerkundung, D-82234 Oberpfaffenhofen, Germany
[4] Harvard & Smithsonian, Ctr Astrophys, 60 Garden St, Cambridge, MA 02138 USA
[5] Free Univ Berlin, Inst Geol Wissensch, Malteserstr 74-100, D-12249 Berlin, Germany
关键词
planets and satellites: terrestrial planets; planets and satellites: detection; planets and satellites: composition; planets and satellites: atmospheres; techniques: spectroscopic; astrochemistry;
D O I
10.1051/0004-6361/202039663
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Context. Terrestrial extrasolar planets around low-mass stars are prime targets when searching for atmospheric biosignatures with current and near-future telescopes. The habitable-zone super-Earth LHS 1140 b could hold a hydrogen-dominated atmosphere, and is an excellent candidate for detecting atmospheric features.Aims. In this study we investigate how the instellation and planetary parameters influence the atmospheric climate, chemistry, and spectral appearance of LHS 1140 b. We study the detectability of selected molecules, in particular potential biosignatures, with the upcoming James Webb Space Telescope (JWST) and Extremely Large Telescope (ELT).Methods. In the first step we used the coupled climate-chemistry model 1D-TERRA to simulate a range of assumed atmospheric chemical compositions dominated by molecular hydrogen (H-2) and carbon dioxide (CO2). In addition, we varied the concentrations of methane (CH4) by several orders of magnitude. In the second step we calculated transmission spectra of the simulated atmospheres and compared them to recent transit observations. Finally, we determined the observation time required to detect spectral bands with low-resolution spectroscopy using JWST, and the cross-correlation technique using ELT.Results. In H-2-dominated and CH4-rich atmospheres oxygen (O-2) has strong chemical sinks, leading to low concentrations of O-2 and ozone (O-3). The potential biosignatures ammonia (NH3), phosphine (PH3), chloromethane (CH3Cl), and nitrous oxide (N2O) are less sensitive to the concentration of H-2, CO2, and CH4 in the atmosphere. In the simulated H-2-dominated atmosphere the detection of these gases might be feasible within 20 to 100 observation hours with ELT or JWST when assuming weak extinction by hazes.Conclusions. If further observations of LHS 1140 b suggest a thin, clear, hydrogen-dominated atmosphere, the planet would be one of the best known targets to detect biosignature gases in the atmosphere of a habitable-zone rocky exoplanet with upcoming telescopes.
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页数:19
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