You Are In The Old Site Archive - Click Here To See The Main Site With Current Stories

Bedrock Is Key To Antarctic Ice Sheet Stability

03.02.2016 13:33 Age: 2 yrs

Geophysicist questions stability of Antarctic Ice Sheet. The ice sheet in the Wilkes Basin may be more stable today than during the in the past because it rests on more bedrock

From the supplementary material to the paper. Computed change in dynamic topography since 3 Ma. (A) Prediction from the Rowley et al. (2013) simulation, and (B) from calculations made by the authors of the recent Geology paper. Courtesy: authors and Geology.


by Rob Enslin, Syracuse University

Robert Moucha, assistant professor of Earth sciences, is the co-author of a recent paper in Geology (Geological Society of America, 2015), examining the impact of the deep Earth on ice-sheet stability. Particular emphasis is on the retreat, or melting, of the East Antarctic Ice Sheet, one of two massive ice sheets in the South Pole and the largest in the world.


Moucha and Harvard Ph.D. candidate Jacquelyn Austermann simulated the 3-million year evolution of convective mantle flow (a process by which the solid Earth cools, causing movement and deformation of its surface), to reconstruct Antarctic bedrock elevation during the mid-Pliocene. The real test, Moucha recalls, was linking their results with mid-Pliocene climate conditions and ice-sheet modeling done by co-authors David Pollard and Robert DeConto at Penn State and the University of Massachusetts Amherst, respectively.

"We found that regions with sub-glacial topography, such as the Wilkes Basin in East Antarctica, were at a lower elevation during the mid-Pliocene," Moucha says. "This had a profound effect on the retreat of the modeled ice-sheet grounding line [the point at which glaciers begin to float, instead of resting on bedrock], raising the global sea-level by a few more meters than would happen in a scenario involving present-day bedrock elevation."


These findings agree with geochemical analyses of offshore sediment cores, suggesting a more retreated ice sheet in the Wilkes Basin, but, until now, they have been difficult to show in ice-sheet simulations. "This implies that the ice sheet in the Wilkes Basin may be more stable today than during the MPWP because it rests on more bedrock," Moucha says.

Given the urgency of this kind of work, he anticipates more interdisciplinary collaborations between tectonicists and climatologists: "It's the tip of the proverbial iceberg, and exemplifies how different disciplines in the Earth sciences can come together to unravel the geological record, while providing a glimpse into the future."

The paper includes authors from Columbia and the universities of Chicago and Quebec.






The impact of dynamic topography change on Antarctic ice sheet stability during the mid-Pliocene warm period by Jacqueline Austermann, David Pollard, Jerry X. Mitrovica, Robert Moucha, Alessandro M. Forte, Robert M. DeConto, David B. Rowley and Maureen E. Raymo published in Geology, doi: 10.1130/G36988.1

Read the abstract and get the paper here.


Syracuse University news release here.