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Webb Finds Atmosphere on Giant Planet Orbiting a White Dwarf

Spectra show hydrocarbons, haze with an unexpectedly warm nightside that modeling links to a reheating event following late inward migration.

Overview

  • The Nature paper, published Wednesday, July 1, reports JWST NIRSpec transit spectroscopy that detected hydrocarbons—most likely methane—small aerosol haze, and a faint thermal glow from the nightside of WD 1856b.
  • WD 1856b is roughly 0.9 times Jupiter’s radius with a mass range of about 4.3–10.9 Jupiter masses, and its eight-minute grazing transit blocks more than half the light of its roughly Earth-sized white dwarf host.
  • The planet’s nightside temperature is estimated near 390–412 K, far hotter than the white dwarf’s light can explain, and cooling-history models date a reheating event to about 3–5.5 billion years after the star became a white dwarf.
  • The team’s modeling favors a late inward migration driven by gravitational interactions in the system’s triple-star architecture but keeps survival through the red-giant phase as an alternative, and four additional JWST transits have been recorded for follow-up analysis.
  • As the first atmospheric measurement of a world orbiting a stellar remnant, this result offers a concrete example for how giant planets may evolve after stellar death while also warning against broad conclusions because the current findings rest on one low-resolution transit.