Detection of the atmosphere of the 1.6 Earth mass exoplanet GJ 1132b

TL;DR

This study reports the first detection of atmospheric features in the low-mass exoplanet GJ 1132b, indicating the presence of atmospheric molecules and expanding understanding of atmospheres in super-Earths.

Contribution

It provides the first evidence of atmospheric features in a low-temperature, low-mass exoplanet, using multi-band transit observations and verification tests.

Findings

Detection of increased radius in z-band suggesting atmospheric presence

Large z-band transit depth indicating strong atmospheric opacity

Atmospheric features compatible with H2O, CH4, or other opacities

Abstract

Detecting the atmospheres of low-mass low-temperature exoplanets is a high-priority goal on the path to ultimately detect biosignatures in the atmospheres of habitable exoplanets. High-precision HST observations of several super-Earths with equilibrium temperatures below 1000K 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 Mearth transiting exoplanet, GJ 1132b, with an equilibrium temperature of ~600K 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 Rearth for the planet, averaged over all the passbands, and a radius of 0.255 +/- 0.023 Rsun 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 Rearth overlaid by atmospheric features which increase the observed radius in the z and K bands. The z-band radius is 4sigma 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 H2O and/or CH4 or a hitherto unconsidered opacity. A surface radius of 1.375 +/- 0.16 Rearth 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 H2O-rich water world.