The JWST weather report from the nearest brown dwarfs III: Heterogeneous clouds and Thermochemical instabilities as possible drivers of WISE 1049AB's spectroscopic variability
Natalia Oliveros-Gomez, Elena Manjavacas, Theodora Karalidi, Myrla Phillippe, Beatriz Campos Estrada, Beth Biller, Johanna M. Vos, Jacqueline Faherty, Xueqing Chen, Trent J. Dupuy, Thomas Henning, Allison M. McCarthy, Philip S. Muirhead, Elspeth K. H. Lee, Pascal Tremblin, Jasmine Ramirez, Genaro Suarez, Ben J. Sutlieff, Xianyu Tan, Nicolas Crouzet
TL;DR
This study uses JWST/NIRSpec time-resolved spectra (0.6–5.3 μm) of the nearby brown-dwarf binary WISE 1049AB to probe the drivers of spectroscopic variability across H2O, CH4, and CO bands. By analyzing molecular-band light curves, their correlations, and depth-dependent contribution functions, the authors show that clouds alone cannot account for the enhanced CH4 and CO variability and that thermochemical instabilities likely play a role, supported by period analyses near the known rotation periods and by 3D-like atmospheric mapping. The results imply a weather system in the L/T transition brown dwarfs where chemical disequilibrium and vertical structure modulate band-specific variability, and they demonstrate the feasibility of constructing atmospheric maps from molecular-band contributions. The work advances our understanding of brown-dwarf atmospheres and demonstrates JWST's capability to disentangle cloud and chemistry-driven variability, with implications for interpreting exoplanetary atmospheres in similar regimes.
Abstract
We present a new analysis of the spectroscopic variability of WISE~J104915.57$-$531906.1AB (WISE~1049AB, L7.5+T0.5), observed using the NIRSpec instrument onboard the James Webb Space Telescope (GO 2965 - PI: Biller). We explored the variability of the dominant molecular bands present in their 0.6--5.3~$μ$m spectra (H$_2$O, CH$_4$, CO), finding that the B component exhibits a higher maximum deviation than the A component in all the wavelength ranges tested. The light curves reveal wavelength-(atmospheric depth) and possibly chemistry-dependent variability. In particular, for the A component, the variability in the light curves at the wavelengths traced by the CH$_4$ and CO molecular absorption features is higher than that of H$_2$O, even when both trace similar pressure levels. We concluded that clouds alone are unlikely to explain the increased variability of CO and CH$_4$ with respect to H$_2$O, suggesting that an additional physical mechanism is needed to explain the observed variability. This mechanism is probably due to thermochemical instabilities. Finally, we provide a visual representation of the 3D atmospheric map reconstructed for both components using the molecular band contributions at different pressure levels and the fit of planetary-scale waves.
