Several firn core records suggest relatively stable accumulation rates during the past two centuries over the Amundsen Sea sector of West Antarctica
Brooke Medley1, Sarah B Das2, Luke D Trusel3, Eric J Steig4, Jan Lenaerts5, Howard Conway4, Joe McConnell6, Michiel R van den Broeke7, Alison S Criscitiello8, David H Bromwich9, Julien P. Nicolas10 and Ian R Joughin11, (1)NASA Goddard Space Flight Center, Greenbelt, MD, United States, (2)Woods Hole Oceanographic Institution, Geology and Geophysics, Woods Hole, United States, (3)Woods Hole Oceanographic Institution, Geology and Geophysics, Woods Hole, MA, United States, (4)University of Washington Seattle Campus, Seattle, WA, United States, (5)University of Colorado Boulder, Department of Atmospheric and Oceanic Sciences, Boulder, CO, United States, (6)Desert Research Institute, Division of Hydrologic Science, Reno, United States, (7)Utrecht University, Institute for Marine and Atmospheric Research, Utrecht, Netherlands, (8)University of Alberta, Department of Earth and Atmospheric Sciences, Edmonton, AB, Canada, (9)Byrd Polar & Climate Rsrch Ctr, Columbus, OH, United States, (10)The Ohio State University, Byrd Polar and Climate Research Center, Columbus, OH, United States, (11)Applied Physics Laboratory, University of Washington, Polar Science Center, Seattle, United States
