Geodynamic modeling of solid Earth – ice sheet – sea level interactions

Predictions of the solid Earth response to changes in ice mass distribution, or glacial isostatic adjustment (GIA), are heavily reliant upon our understanding of the Earth’s viscoelastic structure in polar regions. It is well established that the ice sheet evolution depends on the bedrock elevation and sea level change at the grounding line (where ice goes from sitting on bedrock to floating on the ocean). My current work shows that regional variability in solid Earth structure will impact both sea level and bedrock elevation predictions for ice mass changes in West Antarctica over the next few centuries. This work has implications for improving constraints on the projected sea level contribution of the Antarctic and Greenland Ice Sheets.

Related publications
Observed and predicted horizontal crustal motion at GPS sites deployed on bedrock in W. Antarctica (Lucas et al., 2025)

Seismic investigations of solid Earth structure

Given the expansive ice coverage across Antarctica, seismic studies offer key insight into the tectonic history and geologic structure of the continent. My research characterizing solid Earth structure in Antarctica is focused on better understanding the origin and development of sub-continental tectonic feature, such as the West Antarctic Rift System and Marie Byrd Land dome.

Related publications
Upper mantle anisotropy for Antarctica from shear wave splitting (Lucas et al., 2022).

Environmental seismology

Related publications

Profile across the Foundation Ice Stream grounding line showing the location of icequakes studies in Lucas et al. (2023).