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Stellar Models Also Limit Exoplanet Atmosphere Studies in Emission
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Stellar Models Also Limit Exoplanet Atmosphere Studies in Emission
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Stellar contamination has long been recognized as a major bottleneck in transmission spectroscopy, limiting our ability to accurately characterize exoplanet atmospheres-particularly for terrestrial worlds. In response, significant observational efforts have shifted toward emission spectroscopy as a potentially more robust alternative, exemplified by initiatives such as the 500-hour JWST Rocky Worlds Director's Discretionary Time (DDT) program. However, the extent to which emission spectroscopy may be affected by stellar effects remains mostly unexplored, in stark contrast with the extensiveexploration and mitigation work for transmission spectroscopy. In this study, we assess the impact of imperfect knowledge of stellar spectra on exoplanet atmospheric retrievals from emission spectroscopy. At 12.8 um, none of the considered bare surface types-basalt, ultramafic, Fe-oxidized, and granitoid-can be reliably distinguished when accounting for the 3 sigma model precision between SPHINX and PHOENIX. At 15.0 um, only the granitoid surface is distinguishable from all others above this threshold. These results show that stellar model uncertainty alone substantially limits our ability to constrain surface composition from photometric data, even before including other sources of uncertainty such as stellar radius. Also, we find that current 15 um eclipse depth estimations using different stellar models introduce a 60 ppm difference for M8 and 20 ppm for M5 stars. This model discrepancy leads to a degeneracy in retrieved planetary albedos and weakens constraints on the presence of an atmosphere. We therefore recommend that future JWST secondary eclipse observations systematically include stellar mid-infrared spectroscopy to mitigate these uncertainties.
Forward citations
Cited by 2 Pith papers
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First JWST thermal phase curves of temperate terrestrial exoplanets reveal no thick atmosphere around TRAPPIST-1 b and c
First JWST phase curves of TRAPPIST-1 b and c rule out thick, heat-redistributing atmospheres; b is likely airless, c may retain a tenuous O2 atmosphere.
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Constraints on the possible atmospheres on TRAPPIST-1 b: insights from 3D climate modeling
Airless, thin residual, and hazy-inversion atmospheres all match TRAPPIST-1 b's eclipse and phase curve data, so a single 15 µm eclipse depth is not enough to conclude a planet is airless.
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