Boers, N., Geosciences Department, Laboratoire de Météorologie Dynamique (CNRS and Institute Pierre Simon Laplace, IPSL), École Normale Supérieure and Paris Sciences and Lettres (PSL) Research University, Paris, 75005, France, Research Domain IV–Transdisciplinary Concepts and Methods, Potsdam Institute for Climate Impact Research, Potsdam, 14473, Germany, Grantham Institute, Imperial College, London, SW7 2AZ, United Kingdom; Ghil, M., Geosciences Department, Laboratoire de Météorologie Dynamique (CNRS and Institute Pierre Simon Laplace, IPSL), École Normale Supérieure and Paris Sciences and Lettres (PSL) Research University, Paris, 75005, France, Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, CA 90095, United States; Rousseau, D.-D., Geosciences Department, Laboratoire de Météorologie Dynamique (CNRS and Institute Pierre Simon Laplace, IPSL), École Normale Supérieure and Paris Sciences and Lettres (PSL) Research University, Paris, 75005, France, Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, United States
Recommended Citation:
Boers N.,Ghil M.,Rousseau D.-D.. Ocean circulation; ice shelf; and sea ice interactions explain Dansgaard–Oeschger cycles[J]. Proceedings of the National Academy of Sciences of the United States of America,2018-01-01,115(47)