Rocky planet
Rocky planets are among the most compelling targets in the search for habitable worlds beyond our solar system. Temperate rocky planets orbiting M dwarf stars — the smallest and most common stars in the galaxy — are particularly exciting because their observational accessibility and closer-in habitable zone compared to sun-like stars. However, M dwarfs are also known for intense stellar flares and high-energy radiation that could strip away planetary atmospheres over time, and without an atmosphere to regulate temperature and shield the surface, habitability becomes impossible — making the question of whether these worlds can hold onto their atmospheres one of the most pressing in exoplanet science. Using JWST thermal emission observations, I have measured the dayside emission of GJ 1132b (Xue et al. 2024), shown that GJ 3929b is likely a bare rock (Xue et al. 2025), and found a surprisingly red and cold dayside on TOI-2445b (Xue et al., submitted). I have also contributed to studies of Gl 486b (Mansfield et al. 2024), LTT 1445A b (Wachiraphan et al. 2025), and TOI-1685 b (Luque et al. 2025), as well as population-level tests of which rocky planets around M dwarfs keep their atmospheres (Coy et al. 2025; Ih et al. 2025).
On the hotter end of the rocky planet spectrum, lava worlds and hot super-Earths orbiting very close to their host stars may harbor thick, volatile-rich atmospheres sustained by magma outgassing — offering a very different but equally fascinating window into planetary chemistry and interior-atmosphere interactions. I have worked on several of these hot rocky worlds, including an atmosphere on the ultra-short-period super-Earth HD 3167 b (Coy et al. 2026), a potential atmosphere on the ultrahot TOI-431b (Smith et al. 2026), and the reflective nature of lava worlds seen in TESS phase curves (Coy et al. 2026).


