
Boundary in a protoplanetary disk where a volatile substance condenses from gas to ice.The snow line is the boundary in a protoplanetary disk — the rotating disk of gas and dust around a young star — where a volatile substance, most commonly water, transitions from gas to solid ice. Inside the snow line, temperatures are high enough that water remains vapor; outside, it condenses onto dust grains. This boundary is crucial for planet formation because the presence of ice dramatically increases the solid material available for building planetary cores. The classic snow line for water is typically located at a few astronomical units (AU) from the star, roughly where the asteroid belt lies in our solar system.
The concept was introduced in the 1970s–1980s in the context of solar system formation, with early work by astronomers like A.G.W. Cameron and later refined by models of disk evolution. The term 'snow line' was popularized in the 1990s.
The snow line position depends on the temperature profile of the disk, which is set by stellar radiation, accretion heating, and disk opacity. When the temperature drops below the condensation point of a volatile (e.g., ~150 K for water at typical disk pressures), ice forms on dust grains. This increases the sticking efficiency of particles, accelerating the growth of planetesimals and planetary cores. Different volatiles (CO2, CO, N2) have different snow lines at different radii, creating a layered structure of icy material in the disk.
Observations with ALMA and JWST now directly image snow lines in protoplanetary disks, helping to constrain disk temperatures and predict where planets form.
The water snow line in our solar system is thought to have migrated outward over time as the Sun's luminosity evolved, which may explain the distribution of water in the outer planets.























