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Mapping the Cloud-driven Atmospheric Dynamics and Chemistry of an Isolated Exoplanet Analog with Harmonic Signatures

Title: Mapping the Cloud-driven Atmospheric Dynamics and Chemistry of an Isolated Exoplanet Analog with Harmonic Signatures
Authors: Michael K. Plummer; Francis P. Cocchini; Peter A. Kearns; Allison M. McCarthy; Étienne Artigau; Nicolas B. Cowan; Roman Akhmetshyn; Johanna M. Vos; Evert Nasedkin; Channon Visscher; Björn Benneke; René Doyon; Stanimir A. Metchev; Jason F. Rowe; Genaro Suárez
Source: The Astronomical Journal, Vol 171, Iss 3, p 195 (2026)
Publisher Information: IOP Publishing
Publication Year: 2026
Collection: Directory of Open Access Journals: DOAJ Articles
Subject Terms: Brown dwarfs; T dwarfs; Exoplanet atmospheres; Extrasolar gaseous giant planets; Exoplanet atmospheric variability; Exoplanet atmospheric dynamics; Astronomy; QB1-991
Description: Young planetary-mass objects and brown dwarfs near the L–T spectral transition exhibit enhanced spectrophotometric variability over field brown dwarfs. Patchy clouds, auroral processes, stratospheric hot spots, and complex carbon chemistry have all been proposed as potential sources of this variability. Using time-resolved, low- to mid-resolution spectroscopy collected with the JWST/NIRISS and NIRSpec instruments, we apply harmonic analysis to SIMP J013656.5+093347.3, a highly variable, young, isolated planetary-mass object. Odd harmonics ( k = 3) at pressure levels (≳1 bar) corresponding to iron (Fe) and forsterite (Mg _2 SiO _4 ) cloud formation suggest a potential north–south hemispheric asymmetry in the cloudy, and likely equatorial, regions. We use the inferred harmonics, along with 1D substellar atmospheric models, to map the flux variability by atmospheric pressure level. These vertical maps demonstrate robust interaction between deep convective weather layers and the overlying stratified and radiative atmosphere. We identify distinct time-varying structures in the near-infrared that we interpret as planetary-scale wave-associated (e.g., Rossby or Kelvin) cloud modulation. We detect deviations from bulk (composite) variability in water (maximum signal-to-noise ratio $({\rm{S}}/{{\rm{N}}}_{\max })=14.0$ ), carbon monoxide ( ${\rm{S}}/{{\rm{N}}}_{{\rm{\max }}}=13.0$ ), and methane ( ${\rm{S}}/{{\rm{N}}}_{{\rm{\max }}}=14.9$ ) molecular signatures. Forsterite cloud modulation is anticorrelated with the overlying carbon monoxide and water abundances and correlated with deep methane absorption, suggesting complex interaction between cloud formation, atmospheric chemistry, and temperature structure. Furthermore, we identify distinct harmonic behavior between methane and carbon monoxide absorption bands, providing evidence for time-resolved disequilibrium carbon chemistry. At the lowest pressures (≲100 mbar), we find that the mapped methane lines transition from absorption to emission, supporting evidence of ...
Document Type: article in journal/newspaper
Language: English
Relation: https://doi.org/10.3847/1538-3881/ae4225; https://doaj.org/toc/1538-3881; https://doaj.org/article/cab5b223c9954b49906e6c08998e9bd7
DOI: 10.3847/1538-3881/ae4225
Availability: https://doi.org/10.3847/1538-3881/ae4225; https://doaj.org/article/cab5b223c9954b49906e6c08998e9bd7
Accession Number: edsbas.3395528D
Database: BASE