Surface Processes and Coupling with Planetary Interiors

Scientists boarding D/V JOIDES Resolution off New Jersey in 1993. Sea level in an ice-free world would be 66 meters (216.5 feet) higher than now—shoulder-high to the Statue of Liberty. Image credit: Kenneth G. Miller, James V. Browning, and Gregory S. Mountain

How do surface processes shape the environment we live in, and how do they interact with the solid Earth interior, with implications for planetary evolution and habitability?

My work on surface processes and interior-surface coupling focuses on:

Predicted (left) and observed (right) sea levels caused by melting of the Greenland Ice Sheet (GrIS). A statistically significant correlation between the two fields (P < 0.001) provides an unambiguous observational detection of the near-field sea level fingerprint of recent GrIS melting in our warming world. Graphic: Coulson, et al., 2022 / Science