I have intensively worked on theoretical modeling of exoplanetary atmospheres, including cloud/haze microphysics, chemistry, radiative transfer, and dynamics. I aim to figure out what physical and chemical processes are working in exoplanetary atmospheres and to establish a way to properly constrain the atmospheric properties from spectroscopic observations.
Observational efforts in the last decade revealed that exoplanetary atmospheres are ubiquitously veiled by clouds/hazes that greatly impact observable atmospheric spectra as well as atmospheric properties (e.g., temperature) themselves. It remains highly uncertain how those exotic particles form, what physical/chemical properties they have, how they interact with a background atmosphere, and how they affect atmospheric observations. I have tackled these questions using a microphysical model of cloud/haze formation.
James Webb Space Telescope (JWST) has started to explore exoplanetary atmospheres and revolutionize our understanding on their physical and chemical properties. I am joining JWST Transiting Exoplanet Community Early Release Science (ERS) team and MANATEE MIRI-NIRCam GTO team to facilitate the interpretation of beautiful JWST data from modeling perspective.
Chemistry is a main driver of shaping the observable atmospheric spectrum. For properly extracting the information of bulk atmospheric compositions such as C/O and N/O ratio, it is necessary to understand atmospheric chemistry. I have worked on analyzing a photochemical model to establish a comprehensive understanding on the link between bulk compositions to "observable compositions" of upper atmospheres.
Atmospheric circulation controls the energy transport and thus temperature of observable atmospheres. The circulation could be greatly different from that of conventional tidally-locked synchronized exoplanets once the planets orbit far way from the central star. Planetary obliquity is one of the critical parameters of such non-synchronized exoplanets, as it induces the seasonality in the circulation. I worked on studying the thermal structures of such tilted exoplanets using a 2D shallow water model.
Several exoplanets are known to have peculiar properties, such as anomalously low apparent density and extremely steep spectral slope in transmission spectrum, which standard theory struggles to explain. One potential solution for those observations is the presence of circumplanetary ring, like what all giant planets in the solar system retain. I have developed a framework to compute the atmospheric spectrum of ringed exoplanet and applied the model to several peculiar exoplanets.
I am recently working on modeling planet formation in protoplanetary disks to establish a connection between atmospheric observations and planet formation theory in the era of the JWST.
Thermal structure of protoplanetary disk is a key to control the compositions of formed planets. Recent ALMA observations revealed prevalence of ring-like sub-structure, hinting the prevalence of dust trap in protoplanetary disks. Such dust trap was suggested to cast shadow on the disk to greatly alter the temperature. I have worked on modeling the thermal and chemical structure of such shadowy disk and found that the shadow may explain the peculiar atmospheric compositions of Jupiter in our Solar System.
More results are (hopefully) coming soon!
Atmospheres on solar system planets/objects are ubiquitously veiled by clouds and hazes. They provide unique opportunity to test our current understanding on the cloud/haze formation processes thanks to extensive observational constrains. I investigated haze formation processes on Triton, the largest moon of Neptune, that hosts nitrogen-dominated atmosphere as similar to Titan and Pluto that host photochemically produced aerosols.