Zhang, J., Center for Climatic Research, University of Wisconsin–Madison, Madison, WI 53706, United States, Department of Atmospheric and Oceanic Sciences, University of Wisconsin–Madison, Madison, WI 53706, United States, Computational Physics and Methods (CCS-2), Center for Nonlinear Studies (CNLS), Los Alamos National Laboratory, Los Alamos, NM 87545, United States; Liu, Z., Center for Climatic Research, University of Wisconsin–Madison, Madison, WI 53706, United States, Department of Atmospheric and Oceanic Sciences, University of Wisconsin–Madison, Madison, WI 53706, United States, Atmospheric Science Program, Department of Geography, Ohio State University, Columbus, OH 43210, United States; Brady, E.C., Climate and Global Dynamics Division, National Center for Atmospheric Research, Boulder, CO 80307, United States; Oppo, D.W., Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, United States; Clark, P.U., College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, United States; Jahn, A., Department of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, CO 80309, United States, Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, United States; Marcott, S.A., Department of Geoscience, University of Wisconsin–Madison, Madison, WI 53706, United States; Lindsay, K., Climate and Global Dynamics Division, National Center for Atmospheric Research, Boulder, CO 80307, United States
Recommended Citation:
Zhang J.,Liu Z.,Brady E.C.,et al. Asynchronous warming and δ18O evolution of deep Atlantic water masses during the last deglaciation[J]. Proceedings of the National Academy of Sciences of the United States of America,2017-01-01,114(42)