Our geographers are part of international team looking at the possible fate of the West Antarctic Ice Sheet in our warming world.
The West Antarctic Ice Sheet is vast and holds enough ice to raise global sea level by 4-5 metres if it melts completely.
The ice sheet is protected on one side by the Ross Ice Shelf, the world’s largest floating ice mass.
This serves as a buttress slowing the flow of glaciers and ice streams towards the sea.
As our climate warms, the Ross Ice Shelf is becoming increasingly vulnerable.
Scientists want to know what global temperature increase would trigger unsustainable melting of the shelf, and the subsequent loss of the ice sheet.
The international team is from the SWAIS2C (Sensitivity of the West Antarctic Ice Sheet to 2°C) project.
It is drilling for a series of cylindrical samples of mud and rocks from the bedrock deep beneath 500 metres of ice.
These samples are expected to contain layers of sediment laid down within the past 23 million years.
This includes periods in Earth’s history when temperatures were warmer than they are today – telling us how higher temperatures could make the ice sheet react in future.
Our geographers, led by Professor Mike Bentley, will analyse the samples to see how the Ross Ice Shelf responded to past warming.
They will be looking for tiny grains of sand holding chemical clues to their history in the form of cosmogenic isotopes.
If past warming caused the West Antarctic Ice Sheet to collapse it will have exposed mountains under the ice, leading to the formation of these rare chemicals.
Mike will examine the sediment taken by the SWAIS2C field team for evidence of the isotopes in grains of sand formed when the mountains eroded.
Alongside our work, SWAIS2C will also search for tiny microfossils of marine algae – organisms that need light to survive – in the samples.
Their presence would point to open ocean conditions in the past and suggest that the Ross Ice Shelf had previously retreated.
The evidence will help scientists piece together a picture of past ice sheet behaviour in West Antarctica.
This will inform models looking at the future of the ice sheet, how fast, when and how much of it might melt, and the impact on global sea level rises.