Atmospheric composition of cold super-Earths

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Scientific paper

Planets of masses below 10 times that of Earth (so-called Super-Earths) orbiting far away from their central star have been discovered by Microlensing surveys. Super-Earth atmospheres cannot be characterized remotely yet. However, based on climate modelling and analogies with our solar system, we can put constraints on possible atmospheric compositions. Whenever the triple point of a gaseous constituent is reached on the surface, this constituent is likely to freeze out until equilibrium between ice and vapour/liquid is reached. Important greenhouse gases which are essential for habitability considerations are water (triple point 6.5 mb, 273 K) and carbon dioxide (triple point 5.18 bar, 216 K). In our work we apply a 1D radiative-convective model to Super-Earth atmospheres. We investigate the effect of varying orbital distance, stellar type and planetary mass upon the ability of water and carbon dioxide to remain in the atmosphere. Our results indicate a threshold regime where atmospheres switch from being CO2-rich to being N2-dominated. Implications for habitability and surface conditions are discussed.

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