I'm a Postdoctoral Research Associate working with Prof. Marianne Haseloff in the Glacier and Ice Sheet Dynamics Group at the Department of Geoscience, University of Wisconsin-Madison. I received my PhD in Geoscience in August 2023 as a part of Prof. Ken Ferrier's Surface Processes and Sea Level Group at UW-Madison. With dual training in galciology and geomorphology, I am pursuing emerging and cross-disciplinary research themes aimed to advance our understanding of the fundamental physical processes that shape Earth's Critical Zone and Cryosphere, two crucial components of Earth's dynamic surface and climate system. 

My PhD thesis focuses on quantifying the physical and chemical processes operating in Earth’s Critical Zone that generate soil and shapes topography. I measured the sensitivity of soil chemical erosion and soil production to climate and dust deposition along a steep climate gradient spanning nearly 3 km in elevation at San Jacinto Mountain in California, the largest vertical relief in a uniform granitic lithology in the contiguous United States. As a part of my PhD research, I also investigated drainage divide migration and river basin reorganization at Qilian Shan, northeast Tibet and San Jacinto Mountain.

I switched gears from digging soils to playing with ice and math as a postdoc to pursue my deep interests in the physics behind the multiway connection between ice sheets, climate, topography, sea level, and solid earth, one of the main themes of long-term Earth system evolution. My current postdoc work focuses on using mathematical ice sheet models to understand the dynamics of water-terminating glaciers and ice sheets and its response to climate and non-climate forcings. I simulate how the grounding line and ice flow dynamics of the Lake Superior Lobe of the Laurentide Ice Sheet responds to rapid lake level drops in a warming climate during last deglaciation. My postdoc work is a part of a larger collaborative research effort to understand how ice sheets, rivers, lakes, and solid Earth interacted to shape the continental landscape of the Lake Superior Basin.