FN Archimer Export Format PT J TI The penultimate deglaciation: protocol for Paleoclimate Modelling Intercomparison Project (PMIP) phase 4 transient numerical simulations between 140 and 127 ka, version 1.0 BT AF Menviel, Laurie Capron, Emilie Govin, Aline Dutton, Andrea Tarasov, Lev Abe-Ouchi, Ayako Drysdale, Russell N. Gibbard, Philip L. Gregoire, Lauren He, Feng Ivanovic, Ruza F. Kageyama, Masa Kawamura, Kenji Landais, Amaelle Otto-Bliesner, Bette L. Oyabu, Ikumi Tzedakis, Polychronis C. Wolff, Eric Zhang, Xu AS 1:1;2:2,3;3:4;4:5;5:6;6:7;7:8,9;8:10;9:11;10:12;11:11;12:4;13:13,14,15;14:4;15:16;16:13;17:17;18:18;19:19,20; FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:; C1 Climate Change Research Center, PANGEA, the University of New South Wales, Sydney, Australia Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, Tagensvej 8, 2100 Copenhagen, Denmark British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK Laboratoire des Sciences du Climat et de l'Environnement (LSCE), Institut Pierre Simon Laplace (IPSL), CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-Sur-Yvette, 91190, France Department of Geological Sciences, University of Florida, P.O. Box 112120, Gainesville, FL 32611, USA Department of Physics and Physical Oceanography, Memorial University of Newfoundland, St John's, Canada Atmosphere and Ocean Research Institute, The University of Tokyo, Tokyo, Japan School of Geography, The University of Melbourne, Melbourne, Australia Laboratoire EDYTEM UMR CNRS 5204, Université Savoie Mont Blanc, 73376 Le Bourget du Lac, France Scott Polar Research Institute, University of Cambridge, Cambridge, CB2 1ER, UK School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK Center for Climatic Research, Nelson Institute for Environmental Studies, University of Wisconsin-Madison, Madison, WI 53706, USA National Institute of Polar Research, Research Organizations of Information and Systems, 10-3 Midori-cho, Tachikawa, Tokyo 190-8518, Japan Department of Polar Science, Graduate University for Advanced Studies (SOKENDAI), 10-3 Midori-cho, Tachikawa, Tokyo 190-8518, Japan Institute of Biogeosciences, Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushima-cho, Yokosuka 237-0061, Japan Climate and Global Dynamics Laboratory, National Center for Atmospheric Research (NCAR), Boulder, CO 80305, USA Environmental Change Research Centre, Department of Geography, University College London, London, UK Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, UK Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, 27570 Bremerhaven, Germany Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou, 730000, China C2 UNSW, AUSTRALIA UNIV COPENHAGEN, DENMARK BRITISH ANTARCTIC SURVEY (BAS), UK LSCE, FRANCE UNIV FLORIDA, USA UNIV MEM NEWFOUNDLAND, CANADA UNIV TOKYO, JAPAN UNIV MELBOURNE, AUSTRALIA UNIV SAVOIE MONT BLANC, FRANCE UNIV CAMBRIDGE, UK UNIV LEEDS, UK UNIV WISCONSIN, USA NATL INST POLAR RES, JAPAN UNIV GRAD ADV STUDIES, JAPAN JAMSTEC, JAPAN NCAR, USA UNIV COLL LONDON, UK UNIV CAMBRIDGE, UK INST A WEGENER, GERMANY UNIV LANZHOU, CHINA IN DOAJ IF 5.24 TC 26 UR https://archimer.ifremer.fr/doc/00511/62284/66502.pdf https://archimer.ifremer.fr/doc/00511/62284/66503.zip https://archimer.ifremer.fr/doc/00511/62284/66504.pdf https://archimer.ifremer.fr/doc/00511/62284/66505.zip LA English DT Article CR IMAGES 1-MD101 IMAGES 3-IPHIS-MD106 MD 123 / GEOSCIENCES 1 MD 125 / SWIFT BIS-CARHOT BO Marion Dufresne AB The penultimate deglaciation (PDG, ∼138–128 thousand years before present, hereafter ka) is the transition from the penultimate glacial maximum (PGM) to the Last Interglacial (LIG, ∼129–116 ka). The LIG stands out as one of the warmest interglacials of the last 800 000 years (hereafter kyr), with high-latitude temperature warmer than today and global sea level likely higher by at least 6 m. Considering the transient nature of the Earth system, the LIG climate and ice-sheet evolution were certainly influenced by the changes occurring during the penultimate deglaciation. It is thus important to investigate, with coupled atmosphere–ocean general circulation models (AOGCMs), the climate and environmental response to the large changes in boundary conditions (i.e. orbital configuration, atmospheric greenhouse gas concentrations, ice-sheet geometry and associated meltwater fluxes) occurring during the penultimate deglaciation. A deglaciation working group has recently been set up as part of the Paleoclimate Modelling Intercomparison Project (PMIP) phase 4, with a protocol to perform transient simulations of the last deglaciation (19–11 ka; although the protocol covers 26–0 ka). Similar to the last deglaciation, the disintegration of continental ice sheets during the penultimate deglaciation led to significant changes in the oceanic circulation during Heinrich Stadial 11 (∼136–129 ka). However, the two deglaciations bear significant differences in magnitude and temporal evolution of climate and environmental changes. Here, as part of the Past Global Changes (PAGES)-PMIP working group on Quaternary interglacials (QUIGS), we propose a protocol to perform transient simulations of the penultimate deglaciation under the auspices of PMIP4. This design includes time-varying changes in orbital forcing, greenhouse gas concentrations, continental ice sheets as well as freshwater input from the disintegration of continental ice sheets. This experiment is designed for AOGCMs to assess the coupled response of the climate system to all forcings. Additional sensitivity experiments are proposed to evaluate the response to each forcing. Finally, a selection of paleo-records representing different parts of the climate system is presented, providing an appropriate benchmark for upcoming model–data comparisons across the penultimate deglaciation. PY 2019 PD AUG SO Geoscientific Model Development SN 1991-959X PU Copernicus GmbH VL 12 IS 8 UT 000482520600002 BP 3649 EP 3685 DI 10.5194/gmd-12-3649-2019 ID 62284 ER EF