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Abstract: A Record of Changes in Southern Hemisphere Atmospheric OH Abundance from <sup>14</sup>CO in Glacial Firn and Ice (Law Dome, Antarctica, 1870 – present AD) (AGU25)

A Record of Changes in Southern Hemisphere Atmospheric OH Abundance from 14CO in Glacial Firn and Ice (Law Dome, Antarctica, 1870 – present AD)

Peter D Neff1,2, Vasilii V Petrenko3, David M Etheridge4,5, Andrew Milford Smith6, Christo Buizert7, Lee T Murray3, Cathy M Trudinger4,5, Mingjian Shi2, Edward Crosier2, Benjamin Hmiel2,8, David Thornton4, Lenneke M Jong5,9, Tas D van Ommen5,9, Mark Curran5,9, Ross Beaudette10, Christina M Harth10, Ray Leonard Langenfelds4, Blagoj Mitrevski4, Michael Dyonisius11, Jessica Ng12, Jeffrey P Severinghaus13 and Ray F Weiss14, (1)University of Minnesota Twin Cities, St. Paul, United States, (2)University of Rochester, Department of Earth and Environmental Sciences, Rochester, United States, (3)University of Rochester, Department of Earth and Environmental Sciences, Rochester, NY, United States, (4)CSIRO Environment, Aspendale, Australia, (5)Australian Antarctic Program Partnership, University of Tasmania, Hobart, Australia, (6)Centre for Accelerator Science, Australian Nuclear Science and Technology Organisation (ANSTO), Lucas Heights, Australia, (7)Oregon State University, Corvallis, OR, United States, (8)Colorado Department of Public Health and Environment, Denver, United States, (9)Australian Antarctic Division, Hobart, Australia, (10)University of California San Diego, Scripps Institution of Oceanography, La Jolla, CA, United States, (11)Niels Bohr Institute, København Ø, Denmark, (12)University of California San Diego, Scripps Institution of Oceanography, La Jolla, United States, (13)Scripps Institution of Oceanography, La Jolla, United States, (14)Univ California San Diego, La Jolla, CA, United States