* Astronomy

Detection of an atmosphere around the super-Earth 55 Cancri e
http://arxiv.org/abs/1511.08901

Before the discovery of extrasolar planets, super-Earths belonged in the realm of science fiction. However, they appear to constitute the most common planetary type in our galaxy. We know very little about these planets beyond very basic planetary and orbital parameters. The WFC3 camera onboard the HST has enabled the spectroscopic observations of the atmospheres of two super-Earths, GJ1214b and HD97658b, with unprecedented precision; but the published spectra of these two objects are featureless, suggesting an atmosphere covered by thick clouds or made of molecular species much heavier than hydrogen. We report here the analysis of the observations performed with the WFC3 of a third, very hot, super-Earth, 55 Cancri e. Given the brightness of 55 Cancri, the observations were obtained in scanning mode, adopting a very long scanning length and a very high scanning speed. These observational parameters are coupled with the geometrical distortions of the instrument, so we have developed a specialized pipeline to de-correlate the signal from the systematics. We measure the transit depth per wavelength channel with an average relative uncertainty of 21 ppm and find a spectral modulation of about 100 ppm. These results suggest that 55 Cancri e is surrounded by an atmosphere, which is hydrogen-rich. Our fully Bayesian spectral retrieval code, TauREx, has identified HCN to be one of the possible trace gases in the atmosphere. While additional observations in a broader wavelength range will be needed to confirm the HCN detection, we discuss here the implications of such result. We adopt a chemical scheme developed with combustion specialists and validated by a wide range of experiments. Our chemical model indicates that a relatively high mixing ratio of HCN would reveal a high C/O ratio, suggesting the atmosphere of 55 Cancri e is a carbon-rich environment.
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Title: Variability in the super-Earth 55 Cnc e
Author: Brice-Olivier Demory, Michael Gillon, Nikku Madhusudhan, Didier Queloz

onsiderable progress has been made in recent years in observations of atmospheric signatures of giant exoplanets, but processes in rocky exoplanets remain largely unknown due to major challenges in observing small planets. Numerous efforts to observe spectra of super-Earths, exoplanets with masses of 1-10 Earth masses, have thus far revealed only featureless spectra. In this paper we report a 4-sigma detection of variability in the dayside thermal emission from the transiting super-Earth 55 Cancri e. Dedicated space-based monitoring of the planet in the mid-infrared over eight eclipses revealed the thermal emission from its dayside atmosphere varying by a factor 3.7 between 2012 and 2013. The amplitude and trend of the variability are not explained by potential influence of star spots or by local thermal or compositional changes in the atmosphere over the short span of the observations. The possibility of large scale surface activity due to strong tidal interactions possibly similar to Io, or the presence of circumstellar/circumplanetary material appear plausible and motivate future long-term monitoring of the planet.

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First puffy, 'warm Jupiter' spotted

Wrapped up snug in a warm, puffy atmosphere, the gas giant planet 55 Cancri b may not realise it is living on the edge.
But it turns out the planet is at just the right distance from its star for its gassy covering to start slipping away. The discovery of this slowly evaporating exoplanet could help us better understand atmospheres in our solar system, including why some worlds have them while others don't.
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Title: A Possible Carbon-rich Interior in Super-Earth 55 Cancri e
Authors: Nikku Madhusudhan (Yale Univ.), Kanani K. M. Lee (Yale Univ.), Olivier Mousis (CNRS, France)

Terrestrial planets in the solar system, such as the Earth, are oxygen-rich, with silicates and iron being the most common minerals in their interiors. However, the true chemical diversity of rocky planets orbiting other stars is yet unknown. Mass and radius measurements are used to constrain the interior compositions of super-Earths (exoplanets with masses of 1 - 10 Earth masses), and are typically interpreted with planetary interior models that assume Earth-centric oxygen-rich compositions. Using such models, the super-Earth 55 Cancri e (mass of 8 Earth masses, radius of 2 Earth radii) has been suggested to bear an interior composition consisting of Fe, silicates, and an envelope (>= 10% by mass) of super-critical water. We report that the mass and radius of 55 Cancri e can also be explained by a carbon-rich solid interior made of Fe, C, SiC, and/or silicates and without a volatile envelope. While the data allow Fe mass fractions of up to 40%, a wide range of C, SiC and/or silicate mass fractions are possible. A carbon-rich 55 Cancri e is also plausible if its protoplanetary disk bore the same composition as its host star, which has been reported to be carbon-rich. However, more precise estimates of the stellar elemental abundances and observations of the planetary atmosphere are required to further constrain its interior composition. The possibility of a C-rich interior in 55 Cancri e opens a new regime of geochemistry and geophysics in extraterrestrial rocky planets, compared to terrestrial planets in the solar system.

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