DOMINOS (Disintegration of Marine Ice Sheets: Novel Optimized Simulations)

Lead Research Organisation: University of St Andrews
Department Name: Geography and Sustainable Development

Abstract

There is growing consensus that Thwaites Glacier, West Antarctica, is unstable and vulnerable to collapse. However, there is significant disagreement in projections of rates of mass loss, with some studies suggesting century to millennial scale retreat and others forecasting more catastrophic disintegration. These disagreements are significant because rapid disintegration of Thwaites and adjacent glaciers could potentially trigger or accelerate collapse of significant portions of the West Antarctic Ice Sheet with implications for global mean sea level rise (SLR) in the coming decades. Predicting rates of ice loss from Thwaites Glacier is currently hampered by a lack of reliable models of ice fracture and breakaway (iceberg calving) and the interactions between calving and climate change. Our study addresses this major knowledge gap, and is motivated by the need to improve sea level projections critical for policy and planning.

Projected rates of sea level rise from the West Antarctic Ice Sheet (and Thwaites Glacier in particular) have large uncertainties due to difficulties in understanding and projecting the calving and dynamic processes that control the ice sheet stability. This uncertainty is magnified by the poorly understood connection between calving processes, ice sheet stability and climate. To address these uncertainties, our proposal seeks to explicitly resolve the processes that could cause retreat and collapse of Thwaites Glacier using a novel ice-dynamics model suite. This model suite includes a discrete element model capable of simulating coupled fracture and ice-flow processes, a 3D full Stokes continuum model, and the continental scale ice-dynamics model BISICLES. Ice dynamics models will be coupled to an ocean forcing model suite including simple plume models, intermediate complexity 2-layer ocean models and fully 3D regional ocean models. This hierarchical approach will use high-fidelity process models to inform and constrain the sequence of lower-order models needed to extrapolate improved understanding to larger scales and has the potential to radically reduce uncertainty of rates of marine ice sheet collapse and associated sea level rise. The large-scale modeling approach will be tested and implemented within the open source BISICLES ice dynamics model.

Planned Impact

Our education and outreach strategy has several overlapping strands.

Engagement with under-represented students: The first strand, led by UM, involves proactive outreach to populations that are under-presented within STEM fields. We will recruit undergraduate students from nearby community colleges to participate in summer research programs at the University of Michigan. These community colleges serve an economically diverse set of students and our goal is to recruit students from under-represented backgrounds that have had fewer opportunities to experience research. PI Bassis will serve as the primary mentor for the students, and graduate students or PDRAs will act as secondary mentors. We will also proactively provide each student with career planning, advice about graduate school, and general mentoring tailored to his or her needs. We will monitor this population of students to determine if a research experience played any role in their academic trajectory.

Outreach Ypsilanti Schools: The Ypsilanti school district, although in close geographic proximity to the University of Michigan, has markedly different demographics. Ypsilanti Public Schools have about 4,000 students: 64 percent are African-American, 5 percent are Hispanic. Our goal is to interact with these students as possible by attending local science fairs and career days, to make them aware of career opportunities in STEM and Earth Science.

Schools in UK: Outreach activities from St Andrews will capitalize on the existing impact activities for CALISMO, through the highly successful GeoBus project. FGeoBus delivers NERC science to schools by developing workshops based on research outcomes, but fit to the science curriculum (National 4, 5 and Higher in Curriculum for Excellence, Scotland; key stages 3-5 for the National Curriculum in England, Wales and Northern Ireland). PI Benn and undergraduate interns will develop teaching materials and activities to help pupils understand the impact of greenhouse warming on glaciers, ice sheets and sea levels, and engage them in discussion about the importance of these topics to their lives.

Outreach to stakeholders - increasing community participation: Glaciological and climate research is often motivated by the need for accurate sea level projections to inform policy and planning. However, what scientists assert about the usefulness of their work does not necessarily reflect stakeholder's perceptions of the usability of that work: climate research done with some social end goal in mind often fails to be taken up by the relevant practitioners. Graduate student Elizabeth Ultee is currently examining statements of usefulness made by glaciology/sea-level researchers alongside statements of usability made by practitioners including urban planners, the US National Parks Service and insurance risk analysts to identify gaps and recommend action to make available the information planners need. This will inform best practice to maximize the usefulness of sea level projections in local planning and adaptation plans.
 
Description In this project, we have been conducting detailed computer model experiments to understand how ice fracture and iceberg 'calving' will potentially destabilise the West Antarctic Ice Sheet. Two papers on this process have been published in Nature Communications and Science. Findings have been presented at conferences (EGU, AGU) and public lectures (Royal Scottish Geographical Society, Rotary Club, Antarctic Heritage Trust).

We have also documented accelerating breakup of Thwaites Eastern Ice Shelf, the only remaining grounded floating extension of Thwaites Glacier. We have shown that the breakup was triggered by progressive weakening of the shelf, partly in response to submarine melting. A paper on these findings is in review with The Cryosphere.
Exploitation Route We have derived 'calving laws' and perspectives on marine ice cliff instability that can be adopted by other groups to improve predictions of the impact of climate change.
Sectors Education,Environment

 
Description Our findings - alongside others from the International Thwaites Glacier Collaboration - have been presented to the UK All-Party Parliamentary Group on the Polar Regions, at a briefing in the House of Commons, June 2019. Findings have also been presented at public events, such as the launch of the Sir David Attenburgh.
Sector Education,Environment
 
Title Animation of Thwaites Glacier ice base and surface elevation profiles from June 2011 to November 2020 
Description Thwaites Glacier, West Antarctica. An animated time series plot of 64 profiles of ice base and surface elevation along a flowline based on the mean flow direction. The flowline passes through a region of large elevation change that took place between 2014 and 2017. The work was funded by NERC projects NE/P011365/1 and NE/S006605/1 
Type Of Material Database/Collection of data 
Year Produced 2021 
Provided To Others? Yes  
URL https://data.bas.ac.uk/full-record.php?id=GB/NERC/BAS/PDC/01510
 
Title Thwaites Glacier ice surface elevation change, December 2013 to July 2017, and July 2017 to November 2020 
Description Two maps of surface elevation change for Thwaites Glacier, West Antarctica. Change is in metres between 2013-12-21 and 2017-07-11, and between 2017-07-11 and 2020-11-02. The work was funded by NERC projects NE/P011365/1 and NE/S006605/1. 
Type Of Material Database/Collection of data 
Year Produced 2021 
Provided To Others? Yes  
URL https://data.bas.ac.uk/full-record.php?id=GB/NERC/BAS/PDC/01503
 
Title Thwaites Glacier ice surface elevation profiles from June 2011 to November 2020 
Description Thwaites Glacier, West Antarctica. A time series of 156 profiles of ice surface elevation along a flowline based on the mean flow direction. The flowline passes through a region of large elevation change that took place between 2014 and 2017. The work was funded by NERC projects NE/P011365/1 and NE/S006605/1. 
Type Of Material Database/Collection of data 
Year Produced 2021 
Provided To Others? Yes  
URL https://data.bas.ac.uk/full-record.php?id=GB/NERC/BAS/PDC/01505
 
Title Thwaites Glacier ice surface speed change from January 2012 to January 2021 
Description A map of changes in ice surface speed in metres/year for Thwaites Glacier, West Antarctica, between January 2012 and January 2021. Speeds based on feature tracking of satellite synthetic aperture radar data. The work was funded by NERC projects NE/P011365/1 and NE/S006605/1. 
Type Of Material Database/Collection of data 
Year Produced 2021 
Provided To Others? Yes  
URL https://data.bas.ac.uk/full-record.php?id=GB/NERC/BAS/PDC/01506
 
Title Thwaites Glacier time series ice surface flow speeds at (107.09 W, 75.48 S) from January 2012 to December 2020 
Description A time series of surface ice flow speed at a point on Thwaites Glacier, West Antarctica. The point is on grounded ice and is upstream of a sub-shelf cavity on the west flank of the fast-moving core of Thwaites Glacier. There are a total of 589 points. First column = yyyy-mm-dd, second column = speed in kilometres per year. The work was funded by NERC projects NE/P011365/1 and NE/S006605/1. 
Type Of Material Database/Collection of data 
Year Produced 2021 
Provided To Others? Yes  
URL https://data.bas.ac.uk/full-record.php?id=GB/NERC/BAS/PDC/01507
 
Title Thwaites Glacier time series of surface elevations at (107.09 W, 75.48 S) from January 2012 to November 2020 
Description A time series of surface elevation at a point on Thwaites Glacier, West Antarctica. The point is on grounded ice and is upstream of a sub-shelf cavity on the west flank of the fast-moving core of Thwaites Glacier. There are a total of 88 points. First column = yyyy-mm-dd, second column = elevation in metres. The work was funded by NERC projects NE/P011365/1 and NE/S006605/1. 
Type Of Material Database/Collection of data 
Year Produced 2021 
Provided To Others? Yes  
URL https://data.bas.ac.uk/full-record.php?id=GB/NERC/BAS/PDC/01504
 
Description CSC IT Centre for Science, Helsinki 
Organisation CSC – IT Centre for Science
Country Finland 
Sector Public 
PI Contribution Sharing modelling code and expertise.
Collaborator Contribution Contributions to publications by Jan Åstrom and Thomas Zwinger (both published and in prep/in review)
Impact Benn, D.I., Åström, J.A.N., Zwinger, T., Todd, J.O.E., Nick, F.M., Cook, S., Hulton, N.R. and Luckman, A., 2017. Melt-under-cutting and buoyancy-driven calving from tidewater glaciers: new insights from discrete element and continuum model simulations. Journal of Glaciology, 63(240), pp.691-702. Todd, J., Christoffersen, P., Zwinger, T., Råback, P. and Benn, D.I., 2019. Sensitivity of a calving glacier to ice-ocean interactions under climate change: new insights from a 3-D full-Stokes model. The Cryosphere, 13(6), pp.1681-1694. Benn, Douglas I., and Jan A. Åström. "Calving glaciers and ice shelves." Advances in Physics: X 3, no. 1 (2018): 1513819. Vallot, D., Åström, J., Zwinger, T., Pettersson, R., Everett, A., Benn, D.I., Luckman, A., van Pelt, W.J., Nick, F. and Kohler, J., 2018. Effects of undercutting and sliding on calving: a global approach applied to Kronebreen, Svalbard. The Cryosphere, 12(2), pp.609-625. Åström, J.A. and Benn, D.I., 2019. Effective rheology across the fragmentation transition for sea ice and ice shelves. Geophysical Research Letters, 46(22), pp.13099-13106.
Start Year 2012