Nightside clouds and disequilibrium chemistry on the hot Jupiter WASP-43b
atmospheric chemistry
530 Physics
atmospheric models
Astronomy & Astrophysics
530
Article
cosmologia e scienza dello spazio
[SDU] Sciences of the Universe [physics]
RADIATIVE-TRANSFER
ROTATION-VIBRATION SPECTRUM
GENERAL-CIRCULATION MODEL
disequilibrium chemistry
MOLECULAR LINE LISTS
Science & Technology
Settore FIS/05
Exoplanets
520 Astronomy
500
DAS
COLLISION-INDUCED ABSORPTION
520
exoplanets
[SDU]Sciences of the Universe [physics]
Physical Sciences
COMPUTER-PROGRAM
RAYLEIGH-SCATTERING
MULTIPLE-SCATTERING
exoplanet atmosphere space mission JWST
Settore PHYS-05/A - Astrofisica
BAYESIAN-INFERENCE
Astrophysics - Instrumentation and Methods for Astrophysics
ATMOSPHERIC CIRCULATION
Astrophysics - Earth and Planetary Astrophysics
DOI:
10.1038/s41550-024-02230-x
Publication Date:
2024-04-30T10:01:58Z
AUTHORS (83)
ABSTRACT
AbstractHot Jupiters are among the best-studied exoplanets, but it is still poorly understood how their chemical composition and cloud properties vary with longitude. Theoretical models predict that clouds may condense on the nightside and that molecular abundances can be driven out of equilibrium by zonal winds. Here we report a phase-resolved emission spectrum of the hot Jupiter WASP-43b measured from 5 μm to 12 μm with the JWST’s Mid-Infrared Instrument. The spectra reveal a large day–night temperature contrast (with average brightness temperatures of 1,524 ± 35 K and 863 ± 23 K, respectively) and evidence for water absorption at all orbital phases. Comparisons with three-dimensional atmospheric models show that both the phase-curve shape and emission spectra strongly suggest the presence of nightside clouds that become optically thick to thermal emission at pressures greater than ~100 mbar. The dayside is consistent with a cloudless atmosphere above the mid-infrared photosphere. Contrary to expectations from equilibrium chemistry but consistent with disequilibrium kinetics models, methane is not detected on the nightside (2σ upper limit of 1–6 ppm, depending on model assumptions). Our results provide strong evidence that the atmosphere of WASP-43b is shaped by disequilibrium processes and provide new insights into the properties of the planet’s nightside clouds. However, the remaining discrepancies between our observations and our predictive atmospheric models emphasize the importance of further exploring the effects of clouds and disequilibrium chemistry in numerical models.
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