Credit: David Dahlbüdding
Provided they host thick,
hydrogen-dominated atmospheres, moons orbiting free-floating exoplanets could
retain much of the heat generated deep within their interiors by tidal forces.
Led by David Dahlbüdding at the Max Planck Institute for Extraterrestrial
Physics and Giulia Roccetti at the European Space Agency, a new study predicts
that hydrogen could act as a potent greenhouse gas—potentially providing
habitable conditions for billions of years after their host planets are first
ejected from their stellar systems. The work has been published in Monthly Notices of the Royal
Astronomical Society.
Heat-absorbing hydrogen
Astronomers have now discovered
hundreds of exoplanets drifting through interstellar space, most of them likely
flung from their parent systems by violent gravitational encounters in the
distant past. After ejection, these rogue worlds would likely have become
extremely cold and dark—according to some astronomers, their moons may have
faced more interesting fates.
During the chaos of ejection, a
moon's orbit can become highly elongated, causing it to be repeatedly stretched
and squeezed by its host planet's gravity. Much like Europa and Enceladus in
our own solar system, these tidal forces could generate vast amounts of
internal heat.
If such a moon's atmosphere were
unstable enough for gases to condense into liquid form, most of this tidal heat
would simply radiate into space. But the situation could be very different for
high-pressure atmospheres dominated by hydrogen.
In Earth's present-day atmosphere,
hydrogen molecules (simple pairs of bonded hydrogen atoms) have little warming
effect—but under high pressures, they can absorb heat through a process known
as "collision-induced absorption" (CIA). During fleeting collisions,
hydrogen molecules form supramolecular complexes: temporary assemblies held
together by weak, non-covalent bonds.
These complexes are far better at
absorbing infrared radiation than the bonds within isolated hydrogen molecules
and can rival the absorption of potent greenhouse gases like carbon dioxide and
methane.
As a result, some previous studies
have considered how much of the energy generated inside a moon, or even newly
formed planets, could be trapped efficiently in a thick hydrogen atmosphere. If
this were possible, these atmospheres could heat up without the large-scale
condensation that plagued earlier carbon dioxide–dominated models.
"Such an exomoon could have
surface temperatures sufficient to keep water liquid without a nearby star,
significantly expanding the possibilities for life to emerge in the
universe," Dahlbüdding explains. "But although such moons could even
be detected in the near future, the confirmation and analysis of any atmosphere
may well be impossible for a long time."
Combining calculations
For now, the best way to explore
these exotic environments is through modeling. As Dahlbüdding explains, these
simulations allow researchers to track how a moon's atmosphere and orbit evolve
over billions of years following its planet's ejection.
"We combined accurate
calculations of atmospheric temperatures with feedback on the chemical
composition, mainly through condensation," he says. "This results in
the most realistic—albeit still approximate—simulations of such moons to date."
On top of this, the researchers
incorporated the latest theoretical insights into how exomoon orbits change
over time. "In 2023, a study led by Giulia Roccetti modeled how orbital circularization leads to a decrease in the available tidal heat
over time," Dahlbüdding continues. "Together with these previous
results, we can calculate the maximum time spent in the habitable zone."
Retaining liquid water
The team's calculations reveal that
in the thickest hydrogen-dominated atmospheres considered (reaching 100 times Earth's surface
pressure), the effect of collision-induced absorption would make conditions
both warm and stable enough to sustain liquid water. In some cases, these
habitable conditions could persist for up to 4.3 billion years after the host
planet's ejection—comparable to the current age of Earth.
"The hydrogen not only acts as
a potent greenhouse gas but also as a stable background where more or less
condensing species like methane, ammonia and water vapor can further contribute
to retaining the internal heat," Dahlbüdding says.
Parallels with early Earth
Beyond modeling distant exomoons,
the researchers suggest their findings may also shed light on Earth's own past.
Before life emerged, our planet's atmosphere may have been far richer in hydrogen than it is today, and periodically pressurized
by frequent asteroid impacts—conditions that could have enhanced
collision-induced absorption.
Such environments may have favored
the formation and replication of RNA molecules, ultimately helping to kickstart
the process of evolution.
"Through ongoing discussions, we are connecting our research to the latest advances in the search for the emergence of life on Earth," Dahlbüdding says. "And with our paper, we hope to build this bridge between bio- and astrophysics for other scientists as well."
Source: Moons orbiting wandering exoplanets could be habitable—with one catch

