2011ApJ...734L..13P

We show that collision-induced absorption allows molecular hydrogen to act as an incondensible greenhouse gas and that bars or tens of bars of primordial H₂-He mixtures can maintain surface temperatures above the freezing point of water well beyond the "classical" habitable zone defined for CO₂ greenhouse atmospheres. Using a one-dimensional radiative-convective model, we find that 40 bars of pure H₂ on a three Earth-mass planet can maintain a surface temperature of 280 K out to 1.5 AU from an early-type M dwarf star and 10 AU from a G-type star. Neglecting the effects of clouds and of gaseous absorbers besides H₂, the flux at the surface would be sufficient for photosynthesis by cyanobacteria (in the G star case) or anoxygenic phototrophs (in the M star case). We argue that primordial atmospheres of one to several hundred bars of H₂-He are possible and use a model of hydrogen escape to show that such atmospheres are likely to persist further than 1.5 AU from M stars, and 2 AU from G stars, assuming these planets have protecting magnetic fields. We predict that the microlensing planet OGLE-05-390Lb could have retained an H₂-He atmosphere and be habitable at ∼2.6 AU from its host M star.