Thwaites MELT

Melting at Thwaites grounding zone and its control on sea level

MELT

MELT, “Melting at Thwaites grounding zone and its control on sea level“, is an interdisciplinary collaborative project between five universities and the British Antarctic Survey (BAS) that aims to use autonomous sensors, vehicles (including Icefin), radar, and moorings to monitor the Thwaites ice shelf and grounding line.

Photo of the MELT and Icefin teams and camp at Thwaites Glacier in 2020. Credit: Icefin/ITGC/Dichek
Photo of the MELT and Icefin teams and camp at Thwaites Glacier in 2020. Credit: Icefin/ITGC/Dichek
Photograph of a terrace on the underside of Thwaites Glacier in Antarctica, as taken by Icefin.
Photograph of a terrace on the underside of Thwaites Glacier in Antarctica, as taken by Icefin.

Research

Our goal is to better understand how the ice is flowing, ice-ocean interface dynamics, and the ocean bathymetry (i.e. the sea floor) in this region, with a particular focus on melting rates and dynamics.

Collaboration

As part of MELT and the International Thwaites Glacier Collaboration (ITGC: a collaboration between the U.S.’s National Science Foundation and the U.K.’s Natural Environment Research Council), Icefin has been funded to look at the underside of one of the fastest changing regions in Antarctica – the Thwaites glacier. This field work will be critical to informing our understanding of global climate systems. Thwaites is a massive glacier on the West Antarctic ice sheet, and is about the size of the state of Florida.

Photo of the BAS team deploying the hot water drill at Thwaites Glacier including Paul Anker, Keith Nicholls, James Smith and Peter Davis Credit: Icefin/ITGC/Schmidt
Photo of the BAS team deploying the hot water drill at Thwaites Glacier including Paul Anker, Keith Nicholls, James Smith and Peter Davis Credit: Icefin/ITGC/Schmidt

About Melt

Project Details

Hot water drills will be used to make small holes in the Thwaites ice shelf so Icefin can access the ocean and grounding zone underneath, as well as for placement of the ocean moorings and autonomous sensors that will monitor year-round for the duration of the project.

This data will be used to augment state-of-the-art ocean and ice sheet models for better understanding of how this highly dynamic and sensitive system interacts with global climate cycles so we can better estimate the state of the glacial basin over the coming centuries.

The project is lead by Dr. Keith Nicholls, an oceanographer with the British Antarctic Survey (BAS), and Dr. David Holland, an applied mathematician (with a background in fluid dynamics) at New York University, with co-leads Dr. Eric Rignot from the University of California at Irving, Dr. John Paden with George Mason University, Dr. Sridhar Anandakrishnan out of Pennsylvania State University, and Dr. Britney Schmidt at Cornell University.

Acknowledgements

The Thwaites MELT program was funded by NSF and NERC (co-leads Holland and Nichols). Fieldwork on Thwaites glacier is supported by NSF, USAP, NERC, and the British Antarctic Survey.