Establish whether the SO2 shoreline applies to planets orbiting hotter stars

Determine whether the SO2 shoreline separating detectable and undetectable SO2 as a function of equilibrium temperature and atmospheric metallicity remains valid for planets orbiting hotter stars, and characterize how the host-star spectral energy distribution and the atmospheric pressure range probed by observations alter its location and shape.

Background

The SO2 shoreline framework was developed primarily for warm planets orbiting K-type stars. HD 106315 c instead orbits an F-type star with a substantially different ultraviolet spectrum, making it unclear whether the same temperature–metallicity boundary can be transferred to hotter-host systems.

The authors compute new VULCAN model grids and find that the resulting shorelines differ significantly from those obtained for K-type stellar atmospheres. This motivates resolving whether the shoreline is universal or instead depends on stellar spectral type, chemical-network assumptions, and the pressure levels sampled by transmission spectroscopy.

References

An important question is whether this shoreline remains valid for planets orbiting hotter stars.

JWST-SUPER I: New insights into irradiated warm Neptunes atmospheres from MIRI observations of HD 106315 c  (2609.09893 - Dyrek et al., 9 Sep 2026) in Section 5.5, “SO2 and CS2 shorelines around solar-type stars”