Balancing the risks of Greenland’s melting ice sheet

University of Bristol News (UK): Scientists investigating the geophysical and hydrological conditions beneath the Greenland ice sheet say their analysis will be vital for helping understand how the ice sheet will respond to climate change. Researchers from the University of Bristol, who have carried out extensive fieldwork in Greenland over the past few years, are to lead a series of new experiments, which could yield important information about the wider risks to global sea levels.

Members of the Bristol Glaciology Centre and colleagues from the University’s Faculty of Engineering will work with partners from the universities of Aberystwyth, Cambridge, Edinburgh, Texas, Woods Hole Oceanographic Institution, NASA-Jet Propulsion Laboratory and the Greenland Geological Survey to collate new geophysical data in two complementary projects, the first using ground-based tracers and the second, a suite of airborne observations.

The Bristol-led tracers project will reveal how meltwater generated on the surface of the ice sheet is routed at its base. They will work alongside colleagues from the universities of Edinburgh and Aberystwyth, to tackle the challenging task of tracing water flow over 100 km and in sub-surface rivers with double the discharge of the River Thames. The huge volumes of water generated on the surface of the Greenland Ice Sheet makes it challenging to detect any artificial tracers injected in the water exported as runoff.

Bristol’s Dr Jemma Wadham, who is leading the project said: “We know little about how water flows beneath the Greenland Ice Sheet because the toolkit available to scientists to trace waters under such challenging conditions has been very limited. We aim to employ a new suite of highly sensitive tracing methods, developed in Bristol, to solve this mystery.”

The airborne geophysics project, lead by the University of Cambridge, will focus on ten major outlet glaciers across the ice sheet and will use radar, gravity and magnetic data to characterize the subglacial environment of the glaciers and, in particular, the presence of water and sediment at the bed.

“Together these two projects will provide important insights and new information on the factors that control basal processes and motion beneath the 1-3 km thickness of ice that covers most of Greenland,” said Prof Jonathan Bamber from Bristol….

Grooves in a Greenland glacier, shot by Steve Jurvetson, Wikimedia Commons via Flickr, under the Creative Commons Attribution 2.0 Generic license