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Title: Detection of the Atmosphere of the 1.6 M{sub ⊕} Exoplanet GJ 1132 b

Journal Article · · The Astronomical Journal (Online)
 [1]; ; ;  [2];  [3];  [4]
  1. Astrophysics Group, Keele University, Staffordshire, ST5 5BG (United Kingdom)
  2. Max Planck Institute for Astronomy, Königstuhl 17, D-69117 Heidelberg (Germany)
  3. Institute of Astronomy, University of Cambridge, Madingley Road, Cambridge CB3 0HA (United Kingdom)
  4. Department of Astronomy, Stockholm University, SE-106 91 Stockholm (Sweden)

Detecting the atmospheres of low-mass, low-temperature exoplanets is a high-priority goal on the path to ultimately detecting biosignatures in the atmospheres of habitable exoplanets. High-precision HST observations of several super-Earths with equilibrium temperatures below 1000 K have to date all resulted in featureless transmission spectra, which have been suggested to be due to high-altitude clouds. We report the detection of an atmospheric feature in the atmosphere of a 1.6 M{sub ⊕} transiting exoplanet, GJ 1132 b, with an equilibrium temperature of ∼600 K and orbiting a nearby M dwarf. We present observations of nine transits of the planet obtained simultaneously in the griz and JHK passbands. We find an average radius of 1.43 ± 0.16 R{sub ⊕} for the planet, averaged over all the passbands, and a radius of 0.255 ± 0.023 R{sub ⊙} for the star, both of which are significantly greater than previously found. The planet radius can be decomposed into a “surface radius” at ∼1.375 R{sub ⊕} overlaid by atmospheric features that increase the observed radius in the z and K bands. The z-band radius is 4σ higher than the continuum, suggesting a strong detection of an atmosphere. We deploy a suite of tests to verify the reliability of the transmission spectrum, which are greatly helped by the existence of repeat observations. The large z-band transit depth indicates strong opacity from H{sub 2}O and/or CH{sub 4} or a hitherto-unconsidered opacity. A surface radius of 1.375 ± 0.16 R{sub ⊕} allows for a wide range of interior compositions ranging from a nearly Earth-like rocky interior, with ∼70% silicate and ∼30% Fe, to a substantially H{sub 2}O-rich water world.

OSTI ID:
22863099
Journal Information:
The Astronomical Journal (Online), Vol. 153, Issue 4; Other Information: Country of input: International Atomic Energy Agency (IAEA); ISSN 1538-3881
Country of Publication:
United States
Language:
English