Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.

Site Tools

  • AAAS
  • Subscribe
  • Feedback

Site Search

Search Advanced

Originally published in Science Express on 5 July 2007
Science 10 August 2007:
Vol. 317. no. 5839, pp. 793 - 796
DOI: 10.1126/science.1141038

Reports

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

J. Jouzel,1* V. Masson-Delmotte,1 O. Cattani,1 G. Dreyfus,1 S. Falourd,1 G. Hoffmann,1 B. Minster,1 J. Nouet,1 J. M. Barnola,2 J. Chappellaz,2 H. Fischer,3 J. C. Gallet,2 S. Johnsen,4,5 M. Leuenberger,6 L. Loulergue,2 D. Luethi,6 H. Oerter,3 F. Parrenin,2 G. Raisbeck,7 D. Raynaud,2 A. Schilt,6 J. Schwander,6 E. Selmo,8 R. Souchez,9 R. Spahni,6 B. Stauffer,6 J. P. Steffensen,2 B. Stenni,10 T. F. Stocker,6 J. L. Tison,9 M. Werner,11 E. W. Wolff12

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 reveals the presence of such features with similar amplitudes during previous glacial periods. We suggest that the interplay between obliquity and precession accounts for the variable intensity of interglacial periods in ice core records.

1 Laboratoire des Sciences du Climat et l'Environnement/Institut Pierre Simon Laplace, CEA-CNRS–Université de Versailles Saint-Quentin en Yvelines, CE Saclay, 91191, Gif-sur-Yvette, France.
2 Laboratoire de Glaciologie et Géophysique de l'Environnement, CNRS/Université Joseph Fourier, Boîte Postale 96, 38402, Saint Martin d'Hères, France.
3 Alfred Wegener Institute for Polar and Marine Research, Columbusstrasse, D27568 Bremerhaven, Germany.
4 Department of Geophysics, Juliane Maries Vej 30, University of Copenhagen, DK-2100, Copenhagen, Denmark.
5 Science Institute, University of Reykjavik, Dunhaga 3, Reykjavik 107, Iceland.
6 Physics Institute, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland.
7 Centre de Spectrométrie Nucléaire et de Spectrométrie de Masse/CNRS, Bat 108, 91405, Orsay, France.
8 Department of Earth Sciences, University of Parma, 43100 Parma, Italy.
9 Département des Sciences de la Terre et de l'Environnement, Université Libre de Bruxelles, Brussels, Belgium.
10 Department of Geological, Environmental and Marine Sciences, University of Trieste, 34127 Trieste, Italy.
11 Max Planck Institute for Biogeochemistry, 100164, D7701 Jena, Germany.
12 British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK.

* To whom correspondence should be addressed. E-mail: jean.jouzel{at}lsce.ipsl.fr

Read the Full Text


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
A critical review of Pacific salmon marine research relating to climate.
C. M. Chittenden, R. J. Beamish, and R. S. McKinley (2009)
ICES J. Mar. Sci.
   Abstract »    Full Text »    PDF »
High-resolution palaeoclimatology of the last millennium: a review of current status and future prospects.
P.D. Jones, K.R. Briffa, T.J. Osborn, J.M. Lough, T.D. van Ommen, B.M. Vinther, J. Luterbacher, E.R. Wahl, F.W. Zwiers, M.E. Mann, et al. (2009)
The Holocene 19, 3-49
   Abstract »    PDF »
Facing future climate change: is the past relevant?.
L. Skinner (2008)
Phil Trans R Soc A 366, 4627-4645
   Abstract »    Full Text »    PDF »
Ancient Permafrost and a Future, Warmer Arctic.
D. G. Froese, J. A. Westgate, A. V. Reyes, R. J. Enkin, and S. J. Preece (2008)
Science 321, 1648
   Abstract »    Full Text »    PDF »



To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)