A river runs beneath it: new study discovers a 460-km river under the Antarctica ice sheet
New discovery could be the missing link to climate models
The discovery of a 460 km river under the Antarctica ice sheet could be the missing link to climate models.
A team of researchers led by Dr. Christine Dow, a professor in the department of Geography and Environmental Management and cross-appointed to the Department of Applied Mathematics, discovered the river from a series of airborne radar surveys and modelling. Their findings show the ice sheet's base has more active water flow than previously thought, which could make it more susceptible to changes in climate.
"From satellite measurements, we know which regions of Antarctica are losing ice and how much, but we don't necessarily know why," said Dow, a Waterloo Climate Institute member. "This discovery could be a missing link in our models. We could be hugely underestimating how quickly the system will melt by not accounting for the influence of these river systems."
The Antarctic Weddell Sea region, where this study is based, holds enough ice to raise the sea level globally by 4.3 meters, and the newly discovered river will play a key role in that sea level rise. Dow and her colleagues showed that the large volume of freshwater pumped from the river into the ocean causes enhanced melt at the sensitive region where ice flows into the ocean and begins to float. In the future, if warm air temperatures cause enough surface melt to reach the ice sheet's base, it could tip Antarctica to a Greenland-like state, with much higher volumes of freshwater flowing into the ocean. More freshwater in the river will likely lead to more ice shelf melt, shrinking of the ice sheet, and an increase in ice flow rate. Ultimately, these controls on the flow of the ice into the ocean will determine much of the future sea level rise.
"Only by knowing why ice is being lost can we make models and predictions of how the ice will react in the future under further global heating and how much this could raise global sea levels," Dow said.
Scientific discoveries like this one are crucial for understanding climate change impacts and helping us understand our warming planet.
Learn more about the Faculty of Environment's interdisciplinary undergraduate programs and read Dow's study Antarctic basal environment shaped by high-pressure flow through a subglacial river system published in the journal of Nature Geoscience.
The University of Waterloo acknowledges that much of our work takes place on the traditional territory of the Neutral, Anishinaabeg and Haudenosaunee peoples. Our main campus is situated on the Haldimand Tract, the land granted to the Six Nations that includes six miles on each side of the Grand River. Our active work toward reconciliation takes place across our campuses through research, learning, teaching, and community building, and is centralized within our Office of Indigenous Relations.