Sub-millennial climate variability from high resolution water isotopes in the EDC ice core

• Main Authors: Grisart, Antoine, Casado, Mathieu, Gkinis, Vasileios, Vinther, Bo, Naveau, Philippe, Vrac, Mathieu, Laepple, Thomas, Minster, Bénédicte, Prié, Fréderic, Stenni, Barbara, Fourré, Elise, Steen Larsen, Hans-Christian, Jouzel, Jean, Werner, Martin, Pol, Katy, Masson-Delmotte, Valérie, Hoerhold, Maria, Popp, Trevor, Landais, Amaelle
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2022
• Subjects: article; Verlagsveröffentlichung; EPICA; ice core
• Online Access: https://doi.org/10.5194/egusphere-2022-168; https://noa.gwlb.de/receive/cop_mods_00060815; https://egusphere.copernicus.org/preprints/egusphere-2022-168/egusphere-2022-168.pdf

The EPICA Dome C (EDC) ice core provides the longest continuous climatic record covering the last 800 000 years (800 kyrs). Obtaining homogeneous high resolution measurements and accounting for diffusion provide a unique opportunity to study the evolution of decadal to millennial variability within the past glacial and interglacial periods. We present here a compilation of high resolution (11 cm) water isotopic records with 27 000 δ18O measurements and 7 920 δD measurements (covering respectively 94 % and 27 % of the whole EDC record), including published and new measurements (2 900 for both δ18O and δD) over the last 800 kyrs on the EDC ice core. We show that overlapping measurement series performed over multiple depth ranges over the past 20 years, using different analytical methods and in different laboratories, are consistent within analytical uncertainty, and therefore can be combined to provide a homogeneous data set. A frequency decomposition of the most complete δ18O record and a simple assessment of the possible influence of diffusion on the measured profile shows that the variability during glacial periods at multi-decadal to multi-centennial timescale is higher than variability of the interglacial periods. This analysis shows as well that during interglacial periods characterized by a temperature optimum at its beginning, the multi-centennial variability is the strongest over this temperature optimum.