Transmission spectrum of Venus as a transiting exoplanet

被引:47
|
作者
Ehrenreich, D. [1 ]
Vidal-Madjar, A. [2 ]
Widemann, T. [3 ]
Gronoff, G. [4 ]
Tanga, P. [5 ]
Barthelemy, M. [1 ]
Lilensten, J. [1 ]
Etangs, A. Lecavelier des
Arnold, L. [6 ]
机构
[1] UJF Grenoble 1, CNRS INSU, IPAG, UMR 5274, Grenoble, France
[2] Univ Paris 06, CNRS, Inst Astrophys Paris, UMR 7095, Paris, France
[3] Univ Paris Diderot, UPMC, Observ Paris, LESIA, Meudon, France
[4] NASA, Langley Res Ctr, Sci Directorate, Chem & Dynam Branch, Hampton, VA 23665 USA
[5] Univ Nice Sophia Antipolis, CNRS, Observ Cote Azur, Lab Cassiopee,UMR 6202, Nice, France
[6] CNRS OAMP, Observ Haute Provence, St Michel lObservatoire, France
来源
ASTRONOMY & ASTROPHYSICS | 2012年 / 537卷
关键词
radiative transfer; planets and satellites: atmospheres; astrobiology; planetary systems; scattering; planets and satellites: individual: Venus; MOLECULAR SPECTROSCOPIC DATABASE; HUBBLE-SPACE-TELESCOPE; METAL-RICH ATMOSPHERE; EXTRASOLAR PLANET; RAYLEIGH-SCATTERING; CROSS-SECTION; HD; 189733B; GJ; 1214B; EARTH; ALTITUDE;
D O I
10.1051/0004-6361/201118400
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
On 5-6 June 2012, Venus will be transiting the Sun for the last time before 2117. This event is an unique opportunity to assess the feasibility of the atmospheric characterisation of Earth-size exoplanets near the habitable zone with the transmission spectroscopy technique and provide an invaluable proxy for the atmosphere of such a planet. In this letter, we provide a theoretical transmission spectrum of the atmosphere of Venus that could be tested with spectroscopic observations during the 2012 transit. This is done using radiative transfer across Venus' atmosphere, with inputs from in-situ missions such as Venus Express and theoretical models. The transmission spectrum covers a range of 0.1-5 mu m and probes the limb between 70 and 150 km in altitude. It is dominated in UV by carbon dioxide absorption producing a broad transit signal of similar to 20 ppm as seen from Earth, and from 0.2 to 2.7 mu m by Mie extinction (similar to 5 ppm at 0.8 mu m) caused by droplets of sulfuric acid composing an upper haze layer above the main deck of clouds. These features are not expected for a terrestrial exoplanet and could help discriminating an Earth-like habitable world from a cytherean planet.
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页数:6
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