Eyeball planet


An eyeball planet is a hypothetical type of tidally locked planet, for which tidal locking induces spatial features resembling an eyeball. They are terrestrial planets where liquids may be present, in which tidal locking will induce a spatially dependent temperature gradient. This temperature gradient may therefore limit the places in which liquid may exist on the surface of the planet to ring- or disk-shaped areas.
Such planets are further divided into "hot" and "cold" types, depending on which side of the planet the liquid is present. A "hot" eyeball planet is usually closer to its host star, and the centre of the "eye", facing the star, is made of rock while liquid is present on the opposite side. A "cold" eyeball planet, usually farther from the star, will have liquid on the side facing the host star while the rest of its surface is made of ice and rocks.
Because most planetary bodies have a natural tendency toward becoming tidally locked to their host body for a long enough timeline, eyeball planets may be common and could host life, particularly in planetary systems orbiting red and brown dwarf stars which have lifespans much longer than other main-sequence stars.

Modeling and climate

Scientists use computer models to study how tidally locked planets—those that always show the same side to their star—might behave. These models show that the side facing the star can become extremely hot, while the side in constant darkness can get very cold. This big difference in temperature can shape how water behaves on the planet’s surface.
That’s what gives an "eyeball planet" its name: a hot, dry center, surrounded by a ring of possible water or ice. If the planet has even a thin atmosphere or ocean, heat can spread from the hot side to the cold side. This can create a narrow region along the edge between day and night called the terminator where temperatures are just right for liquid water to exist.
Studies by climate scientists have used general circulation models to simulate these dynamics. These models show that factors like greenhouse gas composition, rotation rate, surface albedo, and cloud formation significantly affect where liquid water can persist.

Potential candidates

is potentially an eyeball planet. The TRAPPIST-1 system may contain several such planets.
According to the observations of the James Webb Space Telescope in 2024, the super-Earth planet LHS 1140b might either have a thin ice shell with a subsurface ocean or an icy surface covered partially in liquid water, the latter of which is an attribute of "cold" eyeball planet.