Welcome! I recently joined the Planetary Science Institute as an Associate Research Scientist.Â
My research interest focus on determining the internal large-scale history and properties of worlds by their external expression (topography, gravity, morphology, etc.).
Caleb Fassett was my postdoc advisor and our works are still going through the review process at a couple of journals. Francis Nimmo was my primary advisor in graduate school. Find PDFs of our published works on Francis' website! For newer (or any) papers feel free to email me for copies.
Are Pluto and Charon representative of Kuiper Belt Objects in terms of their tectonic evolution?
Using spherical harmonics and terrain evolution models unveils how topography is the result of interlinked processes.
The condition of lunar gravity anomalies relative to topography are one of the best ways to constrain the Moon's thermal history.
Channels on the surface of Venus likely formed during transition to its modern climate, but we need to understand them better to be sure.
Did these long channels on the lunar surface form by flowing erosion or collapsed lava tubes?
Craters formed from ejecta reveal crustal property changes across geologic boundaries.