Overview
- Secondary‑eclipse observations show a dayside temperature near 3,200°F (≈1,800°C), far below the ≈4,900°F (≈2,700°C) expected for bare molten rock.
- The results come from JWST General Observers Program 3860, which continuously monitored the TOI‑561 system for more than 37 hours across nearly four orbits.
- The evidence supports a substantial, volatile‑rich atmosphere that best explains the thermal signature and helps account for the planet’s unusually low bulk density.
- Researchers propose a magma–atmosphere equilibrium in which outgassing and reabsorption by the molten interior help the small, highly irradiated planet retain its gases.
- TOI‑561 b is a roughly 1.4‑Earth‑radius, ~2‑Earth‑mass ultra‑short‑period world orbiting an ancient, iron‑poor thick‑disk star, and the team is now analyzing the full dataset to map temperatures and constrain atmospheric composition.