Jupiter as an exoplanet: UV to NIR transmission spectrum reveals hazes, a Na layer, and possibly stratospheric H2O-ice clouds

Currently, the analysis of transmission spectra is the most successful technique to probe the chemical composition of exoplanet atmospheres. However, the accuracy of these measurements is constrained by observational limitations and the diversity of possible atmospheric compositions. Here, we show t...

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Detalhes bibliográficos
Autores: Montañés-Ridríguez, Pilar, González-Merino, B., Pallé, Enric, López-Puertas, Manuel, García Melendo, Enrique José|||0000-0002-3354-1140
Formato: artículo
Fecha de publicación:2015
País:España
Recursos:Universitat Politècnica de Catalunya (UPC)
Repositorio:UPCommons. Portal del coneixement obert de la UPC
Idioma:inglés
OAI Identifier:oai:upcommons.upc.edu:2117/111904
Acesso em linha:https://hdl.handle.net/2117/111904
https://dx.doi.org/10.1088/2041-8205/801/1/L8
Access Level:acceso abierto
Palavra-chave:Extrasolar planets
Jupiter (Planet)
Eclipses
Planets and satellites
Atmospheres
Gaseous planets
Jupiter
Ganymede
Planetes extrasolars
Júpiter (Planeta)
Àrees temàtiques de la UPC::Física::Astronomia i astrofísica
Descrição
Resumo:Currently, the analysis of transmission spectra is the most successful technique to probe the chemical composition of exoplanet atmospheres. However, the accuracy of these measurements is constrained by observational limitations and the diversity of possible atmospheric compositions. Here, we show the UV – VIS – IR transmission spectrum of Jupiter as if it were a transiting exoplanet, obtained by observing one of its satellites, Ganymede, while passing through Jupiter’s shadow, i.e., during a solar eclipse from Ganymede. The spectrum shows strong extinction due to the presence of clouds (aerosols) and haze in the atmosphere and strong absorption features from CH4. More interestingly, the comparison with radiative transfer models reveals a spectral signature, which we attribute here to a Jupiter stratospheric layer of crystalline H2O ice. The atomic transitions of Na are also present. These results are relevant for the modeling and interpretation of giant transiting exoplanets. They also open a new technique to explore the atmospheric composition of the upper layers of Jupiter’s atmosphere.