14CO in Glacial Ice from Law Dome, Antarctica as a Tracer of Changes in Atmospheric OH Abundance from 1870 AD to Present

Peter D Neff1,2, Vasilii V Petrenko1, David M Etheridge3, Andrew M Smith4, Edward Crosier1, David Thornton3, Lenneke M Jong5, Ross Beaudette6, Christina M Harth6, Ray Leonard Langenfelds3, Mark Curran5, Benjamin Hmiel1, Christo Buizert7, Lee T Murray1, Cathy M Trudinger3, Michael Dyonisius1, Jessica Yi-Jun Ng6, Jeffrey P Severinghaus6, Blagoj Mitrevski3 and Ray F Weiss6, (1)University of Rochester, Department of Earth and Environmental Sciences, Rochester, NY, United States, (2)University of Washington, Department of Earth and Space Sciences, Seattle, WA, United States, (3)CSIRO, Aspendale, VIC, Australia, (4)Australian Nuclear Science and Technology Organisation (ANSTO), Kirrawee DC, Australia, (5)Australian Antarctic Division, Kingston, TAS, Australia, (6)Scripps Institution of Oceanography, La Jolla, CA, United States, (7)Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, OR, United States