Global carbon-14 observations constrain rates of soil organic matter decomposition in the Energy Exascale Earth System Model
Paul Alexander Levine1, James Tremper Randerson2, Qing Zhu3, William J Riley4, Alison Hoyt5,6, Susan Trumbore7,8, Zheng Shi9, Steven D Allison2,10 and Dr. Forrest M Hoffman, PhD11, (1)University of California Los Angeles, Los Angeles, United States, (2)University of California Irvine, Earth System Science, Irvine, CA, United States, (3)Lawrence Berkeley National Laboratory, Climate & Ecosystem Sciences Division, Berkeley, CA, United States, (4)Lawrence Berkeley National Laboratory, Berkeley, CA, United States, (5)Stanford University, Earth Systems Science, Stanford, CA, United States, (6)Lawrence Berkeley National Laboratory, Berkeley, United States, (7)Max Planck Institute for Biogeochemistry, Jena, Germany, (8)University of California, Department of Earth System Science, Irvine, United States, (9)University of California Irvine, Department of Earth System Science, Irvine, CA, United States, (10)University of California Irvine, Ecology and Evolutionary Biology, Irvine, United States, (11)Computational Earth Sciences Group and Climate Change Science Institute, Oak Ridge National Laboratory, Oak Ridge, United States
