Milillo's Lab
Cryosphere and ice-sheet dynamics
Where an ice sheet loses contact with its bed, and how fast that boundary is moving.
The problem
The grounding line is the boundary where an ice sheet stops resting on bedrock and begins to float. It is not a line and it does not hold still: it migrates by kilometres over a single tidal cycle, and it retreats over years as warm ocean water reaches further beneath the ice. Its position sets how much ice is exposed to ocean melt, which is why models are so sensitive to it.
How we measure it
We map the grounding zone from short-repeat radar interferometry. One-day and four-day repeat passes from COSMO-SkyMed, TanDEM-X and Sentinel-1 resolve the tidal flexure hinge directly, so migration can be separated from long-term retreat rather than confounded with it.
What we have found
Thwaites Glacier
Retreat of 0.8 km/yr in the fastest sector, with floating ice melting at 200 m/yr, while adjacent sectors retreat at 0.3 km/yr and melt ten times slower.
Pine Island Glacier
The grounding line migrates over a zone 2.5 km wide at tidal frequencies in 2016-2017, against 0.5 km in 1996.
Model gap
Measured retreat rates outpace what coupled ice-sheet and ocean models anticipate on yearly time scales.
Papers on this theme 19
Showing the 12 most relevant of 19. See all 92 publications.
Geophysical Research Letters · 2017
Proceedings of the National Academy of Sciences of the United States of America · 2023
Cryosphere · 2022
Geophysical Research Letters · 2020
International Geoscience and Remote Sensing Symposium (IGARSS) · 2017
Heterogeneous retreat and ice melt of Thwaites Glacier, West Antarctica
Science Advances · 2019
Journal of Geophysical Research: Earth Surface · 2017
Rapid glacier retreat rates observed in West Antarctica
Nature Geoscience · 2022
Proceedings of SPIE – The International Society for Optical Engineering · 2016
Cryosphere · 2025
Remote Sensing of Environment · 2024
Antarctic grounding line delineation from the Italian Space Agency COSMO-SkyMed DInSAR data
Scientific data · 2025