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.

Bedrock Ocean Grounded ice Floating ice shelf Grounding line retreattidal migration warm water intrusion
The grounding line is a zone, not a line. Short-repeat interferometry separates tidal migration (which reverses) from retreat (which does not).

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.

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