Temporal and spatial structure of multi-millennial temperature changes at high latitudes during the Last Interglacial

• Published in: Quaternary Science Reviews
• Main Authors: Capron, Émilie, Govin, Aline, Stone, Emma, J, Masson-Delmotte, Valérie, Mulitza, Stefan, Otto-Bliesner, Bette L., Rasmussen, Tine L., Sime, Louise C., Waelbroeck, Claire, Wolff, Eric W.
• Other Authors: Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Climat et Magnétisme (CLIMAG), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), School of Geographical Sciences Bristol, University of Bristol Bristol, Glaces et Continents, Climats et Isotopes Stables (GLACCIOS), Center for Marine Environmental Sciences Bremen (MARUM), Universität Bremen, National Center for Atmospheric Research Boulder (NCAR), The Arctic University of Norway Tromsø, Norway (UiT), British Antarctic Survey (BAS), Natural Environment Research Council (NERC), Paléocéanographie (PALEOCEAN), Godwin Laboratory, Department of Earth Sciences Cambridge, UK, University of Cambridge UK (CAM)-University of Cambridge UK (CAM)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2014
• Subjects: Last Interglacial period; Ice cores; Marine sediment cores; Data synthesis; Climate model simulations; [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology; Antarctic; Southern Ocean; Antarc*; Antarctica; ice core; North Atlantic
• Online Access: https://hal.science/hal-02180978; https://hal.science/hal-02180978/document; https://hal.science/hal-02180978/file/Capron-QSR2014.pdf; https://doi.org/10.1016/j.quascirev.2014.08.018

International audience The Last Interglacial (LIG, 129e116 thousand of years BP, ka) represents a test bed for climate model feedbacks in warmer-than-present high latitude regions. However, mainly because aligning different palaeoclimatic archives and from different parts of the world is not trivial, a spatio-temporal picture of LIG temperature changes is difficult to obtain. Here, we have selected 47 polar ice core and sub-polar marine sediment records and developed a strategy to align them onto the recent AICC2012 ice core chronology. We provide the first compilation of high-latitude temperature changes across the LIG associated with a coherent temporal framework built between ice core and marine sediment records. Our new data synthesis highlights non-synchronous maximum temperature changes between the two hemispheres with the Southern Ocean and Antarctica records showing an early warming compared to North Atlantic records. We also observe warmer than present-day conditions that occur for a longer time period in southern high latitudes than in northern high latitudes. Finally, the amplitude of temperature changes at high northern latitudes is larger compared to high southern latitude temperature changes recorded at the onset and the demise of the LIG. We have also compiled four data-based time slices with temperature anomalies (compared to present-day conditions) at 115 ka, 120 ka, 125 ka and 130 ka and quantitatively estimated temperature uncertainties that include relative dating errors. This provides an improved benchmark for performing more robust model-data comparison. The surface temperature simulated by two General Circulation Models (CCSM3 and HadCM3) for 130 ka and 125 ka is compared to the corresponding time slice data synthesis. This comparison shows that the models predict warmer than present conditions earlier than documented in the North Atlantic, while neither model is able to produce the reconstructed early Southern Ocean and Antarctic warming. Our results highlight the importance of ...