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  Stability of marine basins in the Antarctic Peninsula Ice Sheet from remote sensing - SENSE CDT


   School of Geosciences

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  Dr R Bingham, Dr A Hogg  No more applications being accepted  Competition Funded PhD Project (Students Worldwide)

About the Project

Introduction and Aim

This project will assess the current and future stability of marine ice-sheet basins that collectively underlie Ellsworth Land, the region that connects the West Antarctic and Antarctic Peninsula Ice Sheets. It is well known that marine ice-sheets basins, defined as the parts of the ice sheets that are grounded below sea level, are particularly vulnerable to retreat and therefore have significant potential to contribute to future global sea-level rise (DeConto and Pollard, 2016; Mercer, 1978), and these processes are much studied in West Antarctica’s Amundsen Sea Embayment (Bingham et al., 2017; Scambos et al., 2017). Despite some studies over the last decade also drawing attention to West Antarctica’s Ellsworth Land also being vulnerable to marine ice-sheet instability (Bingham et al., 2012) and currently showing signs of this being underway (Hogg et al., 2017; Wouters et al., 2015), the region remains relatively data-poor for good estimates of its future retreat rates and sea-level contributions. Addressing this fundamental knowledge gap and elucidating the dangers to near-future sea-level rise posed by potential retreat of ice from Ellsworth Land form the focus of this project.

Aim, objectives and methods of the proposed research

The main aim of the project is to assess the near-term (200 years into the future) stability of the Ellsworth Land marine basin lying between West Antarctica and the Antarctic Peninsula. This comprises the following objectives:

  1. To compile for Ellsworth Land time series of contemporary glaciological change (changes to ice-surface velocity, surface elevation and the grounding line) from Earth Observation datasets;
  2. To track englacial horizons (treated as isochrones, or surfaces of equal age) across Ellsworth Land, and thereby place age constraints on its deep ice, using age constraints from adjacent layer-tracking and links to West Antarctica’s ice core age-depth profiles – with the ultimate aim of constraining what is the oldest ice in the region, and hence give clues to its past stability;
  3. To explore the application of machine-learning methods for tracking englacial layers in geophysical data and/or compiling time series of contemporary changes from Earth Observation data.

This PhD is part of the NERC and UK Space Agency funded Centre for Doctoral Training "SENSE": the Centre for Satellite Data in Environmental Science. SENSE will train 50 PhD students to tackle cross-disciplinary environmental problems by applying the latest data science techniques to satellite data. All our students will receive extensive training on satellite data and AI/Machine Learning and field training. All students will experience extensive training on professional skills, including spending 3 months on an industry placement. See http://www.eo-cdt.org

Application support

As part of our ongoing EDI work, we want to widen participation for UK-domiciled underrepresented groups, which we have identified as Black, Asian and minority ethnic candidates, disabled persons and those from a disadvantaged socio-economic background. As such, we are offering prospective candidates from these groups opportunities and resources such as:

  • This year SENSE are guaranteeing interview slots for up to 50% of our previous year’s interview allocation, for BAME or disabled applicants. Gender is not one of SENSE’s underrepresented categories.
  • 1-2-1 sessions with one of our Centre Managers ([Email Address Removed]) or our EDI Champion to further advise candidates on their applications.

More information for applicants can be found on our available ProjectsHow to Apply and dedicated FAQ webpages. You will also find additional resources such as How can a PhD help me with my career?

Environmental Sciences (13) Geology (18)

Funding Notes

This 3 year 9 month long NERC SENSE CDT award will provide tuition fees, tax-free stipend at the UK research council rate (£17,668 for 2022/23), and a research training and support grant to support national and international conference travel. www.eo-cdt.org/apply-now

References

Bingham, R.G., Ferraccioli, F., King, E.C., Larter, R.D., Pritchard, H.D., Smith, A.M. and Vaughan, D.G., 2012. Inland thinning of West Antarctic Ice Sheet steered along subglacial rifts. Nature, 487(7408): 468-471.
Bingham, R.G., Vaughan, D.G., King, E.C., Davies, D., Cornford, S.L., Smith, A.M., Arthern, R.J., Brisbourne, A.M., De Rydt, J., Graham, A.G.C., Spagnolo, M., Marsh, O.J. and Shean, D.E., 2017. Diverse landscapes beneath Pine Island Glacier influence ice flow. Nature Communications, 8: 1618.
DeConto, R.M. and Pollard, D., 2016. Contribution of Antarctica to past and future sea-level rise. Nature, 531(7596): 591-597.
Hogg, A.E., Shepherd, A., Cornford, S.L., Briggs, K.H., Gourmelen, N., Graham, J.A., Joughin, I., Mouginot, J., Nagler, T., Payne, A.J., Rignot, E. and Wuite, J., 2017. Increased ice flow in Western Palmer Land linked to ocean melting. Geophysical Research Letters, 44(9): 4159-4167.
Mercer, J.H., 1978. West Antarctic ice sheet and CO2 greenhouse effect: a threat of disaster. Nature, 271(5643): 321-325.
Scambos, T.A., Bell, R.E., Alley, R.B., Anandakrishnan, S., Bromwich, D.H., Brunt, K., Christianson, K., Creyts, T., Das, S.B., DeConto, R., Dutrieux, P., Fricker, H.A., Holland, D., MacGregor, J., Medley, B., Nicolas, J.P., Pollard, D., Siegfried, M.R., Smith, A.M., Steig, E.J., Trusel, L.D., Vaughan, D.G. and Yager, P.L., 2017. How much, how fast?: A science review and outlook for research on the instability of Antarctica's Thwaites Glacier in the 21st century. Global and Planetary Change, 153: 16-34.
Wouters, B., Martin-Español, A., Helm, V., Flament, T., van Wessem, J.M., Ligtenberg, S.R.M., van den Broeke, M.R. and Bamber, J.L., 2015. Dynamic thinning of glaciers on the Southern Antarctic Peninsula. Science, 348(6237): 899-903.

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