Antarctic Ice Sheet retreat in the western Ross Embayment since the Last Glacial Maximum constrained by geochronology and ice flow modeling
Trevor Hillebrand1, Courtney King2, Michelle R Koutnik3, John Stone4, Brenda L Hall5, Howard Conway4, David Pollard6, Brent M Goehring7, Keir Alexander Nichols8 and Mette Gillespie9, (1)Los Alamos National Laboratory, Los Alamos, United States, (2)University of Maine, School of Earth and Climate Sciences and Climate Change Institute, Orono, ME, United States, (3)University of Washington, Department of Earth and Space Sciences, Seattle, United States, (4)University of Washington, Department of Earth and Space Sciences, Seattle, WA, United States, (5)University of Maine, Earth and Climate Sciences and Climate Change Institute, Orono, United States, (6)Pennsylvania State University, Earth and Environmental Systems Institute, University Park, PA, United States, (7)Tulane University of Louisiana, Department of Earth and Environmental Sciences, New Orleans, LA, United States, (8)Tulane University of Louisiana, Department of Earth and Environmental Sciences, New Orleans, United States, (9)Western Norway University of Applied Sciences, Sogndal, Norway
