Orbital and Millennial Antarctic Climate Variability over the Past 800,000 Years

@article{Jouzel2007OrbitalAM,
  title={Orbital and Millennial Antarctic Climate Variability over the Past 800,000 Years},
  author={Jean Jouzel and Val{\'e}rie Masson‐Delmotte and Olivier Cattani and Georges Dreyfus and Sonia Falourd and Georg Hoffmann and B{\'e}n{\'e}dicte Minster and J. Nouet and J-M. Barnola and J{\'e}r{\^o}me Chappellaz and Hubertus Fischer and Jean‐Charles Gallet and Sigfús J. Johnsen and Markus Christian Leuenberger and Laetitia Loulergue and Dean Luethi and Hans Oerter and Fr{\'e}d{\'e}ric Parrenin and Grant M. Raisbeck and Dominique Raynaud and A. Schilt and Jakob Schwander and Enrico Selmo and Roland Souchez and Renato Spahni and B. Stauffer and J{\o}rgen Peder Steffensen and Barbara Stenni and Thomas F. Stocker and Jean-Louis Tison and Martin Werner and Eric W. Wolff},
  journal={Science},
  year={2007},
  volume={317},
  pages={793 - 796}
}
A high-resolution deuterium profile is now available along the entire European Project for Ice Coring in Antarctica Dome C ice core, extending this climate record back to marine isotope stage 20.2, ∼800,000 years ago. Experiments performed with an atmospheric general circulation model including water isotopes support its temperature interpretation. We assessed the general correspondence between Dansgaard-Oeschger events and their smoothed Antarctic counterparts for this Dome C record, which… 

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