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Webb Finds Strong Evidence of Thick Atmosphere on Ultra-Hot Super-Earth TOI-561 b

A cooler-than-expected dayside temperature points to a volatile-rich shroud likely sustained by exchange with a global magma ocean.

Overview

  • JWST’s NIRSpec secondary-eclipse measurements put the planet’s dayside near 1,800°C, well below the ~2,700°C expected for a bare rock.
  • The Carnegie-led study, published December 11 in The Astrophysical Journal Letters, reports the strongest evidence yet for an atmosphere on this rocky world.
  • Continuous 37-hour observations in JWST General Observers Program 3860 covered nearly four orbits to produce these first results.
  • Scenarios involving magma heat transport or a thin rock-vapor layer fail to explain the magnitude of the cooling seen in the data.
  • The authors propose an outgassing–reabsorption balance could sustain a long-lived atmosphere under extreme irradiation, with further analysis underway to map temperatures and identify gases.