Details of Award
NERC Reference : NE/S011994/1
Quantifying Human Influence on Ocean Melting of the West Antarctic Ice Sheet
Grant Award
- Principal Investigator:
- Professor PR Holland, NERC British Antarctic Survey, Science Programmes
- Co-Investigator:
- Dr K Kusahara, Japan Agency for Marine-Earth Sci & Tech, UNLISTED
- Co-Investigator:
- Dr S Kimura, Japan Agency for Marine-Earth Sci & Tech, UNLISTED
- Co-Investigator:
- Professor A Jenkins, Northumbria University, Fac of Engineering and Environment
- Co-Investigator:
- Professor A Naveira Garabato, University of Southampton, Sch of Ocean and Earth Science
- Co-Investigator:
- Dr S S Aoki, Hokkaido University, Institute of Low Temperature Science
- Grant held at:
- NERC British Antarctic Survey, Science Programmes
- Science Area:
- None
- Overall Classification:
- Unknown
- ENRIs:
- None
- Science Topics:
- Glacial processes
- Ocean modelling
- Sea level rise
- Climate & Climate Change
- Abstract:
- The West Antarctic Ice Sheet (WAIS) is a huge slab of glacier ice about the size of Europe, and a few kilometres thick. Satellite observations show that the WAIS is losing ice, and this is causing global sea level to rise. If the current rate of ice loss continues, the WAIS alone will cause 50 cm of global sea-level rise by 2100. The ice loss is caused by increased ocean melting beneath areas of floating glacial ice called ice shelves. In the Amundsen Sea region of Antarctica, ocean melting is causing the ice shelves to thin very rapidly. The ultimate cause of these changes in melting is not known. Earth's climate experiences large natural variations, and we know that these variations have a strong influence on the Amundsen Sea. As a result, we don't know whether the increased melting of the WAIS is caused by human-induced climate change, or by natural variability. This project will address that question. Scientists in the UK and Japan are leading the world in developing computer models of the ice and ocean in the Amundsen Sea. We will force these models with a wide range of atmospheric conditions for the past and future, including both natural variability and human-induced changes. These forcings will be taken from global climate model simulations. By considering the results of all these models together, and averaging over many possible examples of the natural variability, we will be able to determine the importance of human-induced changes. In order to be confident in these results, we need to know what ocean processes are causing the model behaviour that we find. We will quantify the importance of different processes by progressively disabling each process in the model and investigating the result. We must also be sure that the models are a good representation of ocean conditions in the region. However, this is difficult because the Amundsen Sea is remote and very poorly observed. To provide the crucial model validation, we will create a new record of ocean currents in the region over the last 25 years, using the latest satellite processing techniques to determine ocean currents even in regions covered by thick sea ice. These results will allow us to determine whether the present ice loss was caused by human activities in the past, and whether melting in the future can be reduced by lower emissions of greenhouse gases. This will enable politicians and the public to decide how best to respond to sea-level rise from the WAIS.
- NERC Reference:
- NE/S011994/1
- Grant Stage:
- Completed
- Scheme:
- RCUK
- Grant Status:
- Closed
- Programme:
- UKRI-JSPS
This grant award has a total value of £507,450
FDAB - Financial Details (Award breakdown by headings)
| DI - Other Costs | Indirect - Indirect Costs | DA - Investigators | DA - Estate Costs | DI - Staff | DA - Other Directly Allocated | DI - T&S |
|---|---|---|---|---|---|---|
| £3,252 | £206,261 | £41,328 | £55,037 | £181,725 | £2,163 | £17,683 |
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