SIMBAD references

JWST has revealed sulfur chemistry in giant exoplanet atmospheres, where molecules such as sulfur dioxide (SO₂) trace photochemistry, metallicity, and formation and migration. To ascertain the conditions that determine whether (or how much) SO₂, H₂S, and other sulfur-bearing species are present in exoplanet atmospheres, we present a grid of planetary atmospheres covering metallicities from 0.3 to 1000× solar and temperatures from 250 to 2050 K. These models map out the “SO₂ shoreline,” the region of metallicity and irradiation for which SO₂ may be sufficiently abundant to be detectable. SO₂ is a sensitive indicator of metallicity; expected SO₂ abundances also depend strongly on overall temperature and C/O ratio; the SO₂ abundance depends surprisingly weakly on X-ray and ultraviolet irradiation, also weakly on K_zz (for T_eq ≳ 600 K), and is essentially independent of internal temperature. Despite its detection in a growing number of giant planets, SO₂ is never the dominant sulfur-bearing molecule: depending on temperature and metallicity, H₂S, S₂, NS, SO, SH, and even S₈ or atomic S are frequently as common (or more so) as SO₂. Nonetheless SO₂ remains the most easily detectable sulfur-bearing species, followed by H₂S, though perhaps SO and SH could be detectable in some gas giants. Aside from a pressing need for additional observational constraints on sulfur, we also identify the need for future work to account for the effects of clouds and hazes, fully self-consistent atmospheric models, 2D and 3D models, a wider range of planetary masses and radii, and studies to measure and refine reaction rates and molecular opacities of sulfur-bearing species.