William is a National Science Foundation Postdoctoral Fellow at Lamont-Doherty Earth Observatory of Columbia University. William's research involves using seismic data to image the interior of the Earth, and integrate geodynamic models with the inferred seismic structure to better understand the long-term evolution of our planet. Although the evolution of oceanic plates plays a crucial role in plate tectonics, and therefore Earth evolution, the structure beneath ocean basins remains largely unexplored. He uses ocean bottom seismometers to address a range of problems in marine geophysics, including deep processes related mid-ocean ridges, structural and mechanical properties of the lithosphere and asthenosphere, and the structure and evolution of subduction zones.
William began at Lamont-Doherty Earth Observatory in the fall of 2019. He completed his PhD at the University of California, Berkeley in 2019, and his B.A. in physics and astrophysics from Harvard University in 2012