Standard
Orbital and millennial Antarctic climate variability over the past 800,000 years. / Jouzel, J.; Masson-Delmotte, V.; Cattani, O.; Dreyfus, G.; Falourd, S.; Hoffmann, G.; Minster, B.; Nouet, J.; Barnola, M.; Chappellaz, J.; Fischer, H.; Gallet, J.C.; Johnsen, Sigfus Johann; Leuenberger, M.; Loulergue, L.; Luethi, D.; Oerter, H.; Parrenin, F.; Raisbeck, G.; Raynaud, D.; Schilt, A.; Schwander, J.; Selmo, E.; Souchez, R.; Spahni, R.; Stauffer, B.; Steffensen, Jørgen Peder; Stenni, B.; Stocker, T.F.; Tison, J.L.; Werner, M.; Wolff, E.W.
In:
Science, Vol. 317, No. 5839, 2007, p. 793-796.
Research output: Contribution to journal › Journal article › Research › peer-review
Harvard
Jouzel, J, Masson-Delmotte, V, Cattani, O, Dreyfus, G, Falourd, S, Hoffmann, G, Minster, B, Nouet, J, Barnola, M, Chappellaz, J, Fischer, H, Gallet, JC, Johnsen, SJ, Leuenberger, M, Loulergue, L, Luethi, D, Oerter, H, Parrenin, F, Raisbeck, G, Raynaud, D, Schilt, A, Schwander, J, Selmo, E, Souchez, R, Spahni, R, Stauffer, B
, Steffensen, JP, Stenni, B, Stocker, TF, Tison, JL, Werner, M & Wolff, EW 2007, '
Orbital and millennial Antarctic climate variability over the past 800,000 years',
Science, vol. 317, no. 5839, pp. 793-796.
https://doi.org/10.1126/science.1141038APA
Jouzel, J., Masson-Delmotte, V., Cattani, O., Dreyfus, G., Falourd, S., Hoffmann, G., Minster, B., Nouet, J., Barnola, M., Chappellaz, J., Fischer, H., Gallet, J. C., Johnsen, S. J., Leuenberger, M., Loulergue, L., Luethi, D., Oerter, H., Parrenin, F., Raisbeck, G., ... Wolff, E. W. (2007).
Orbital and millennial Antarctic climate variability over the past 800,000 years.
Science,
317(5839), 793-796.
https://doi.org/10.1126/science.1141038Vancouver
Jouzel J, Masson-Delmotte V, Cattani O, Dreyfus G, Falourd S, Hoffmann G et al.
Orbital and millennial Antarctic climate variability over the past 800,000 years.
Science. 2007;317(5839):793-796.
https://doi.org/10.1126/science.1141038Author
Jouzel, J. ; Masson-Delmotte, V. ; Cattani, O. ; Dreyfus, G. ; Falourd, S. ; Hoffmann, G. ; Minster, B. ; Nouet, J. ; Barnola, M. ; Chappellaz, J. ; Fischer, H. ; Gallet, J.C. ; Johnsen, Sigfus Johann ; Leuenberger, M. ; Loulergue, L. ; Luethi, D. ; Oerter, H. ; Parrenin, F. ; Raisbeck, G. ; Raynaud, D. ; Schilt, A. ; Schwander, J. ; Selmo, E. ; Souchez, R. ; Spahni, R. ; Stauffer, B. ; Steffensen, Jørgen Peder ; Stenni, B. ; Stocker, T.F. ; Tison, J.L. ; Werner, M. ; Wolff, E.W. / Orbital and millennial Antarctic climate variability over the past 800,000 years. In: Science. 2007 ; Vol. 317, No. 5839. pp. 793-796.
Bibtex
@article{4b44afe001b311deb05e000ea68e967b,
title = "Orbital and millennial Antarctic climate variability over the past 800,000 years",
abstract = "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. Udgivelsesdato: 10.08",
author = "J. Jouzel and V. Masson-Delmotte and O. Cattani and G. Dreyfus and S. Falourd and G. Hoffmann and B. Minster and J. Nouet and M. Barnola and J. Chappellaz and H. Fischer and J.C. Gallet and Johnsen, {Sigfus Johann} and M. Leuenberger and L. Loulergue and D. Luethi and H. Oerter and F. Parrenin and G. Raisbeck and D. Raynaud and A. Schilt and J. Schwander and E. Selmo and R. Souchez and R. Spahni and B. Stauffer and Steffensen, {J{\o}rgen Peder} and B. Stenni and T.F. Stocker and J.L. Tison and M. Werner and E.W. Wolff",
year = "2007",
doi = "10.1126/science.1141038",
language = "English",
volume = "317",
pages = "793--796",
journal = "Science",
issn = "0036-8075",
publisher = "American Association for the Advancement of Science",
number = "5839",
}
RIS
TY - JOUR
T1 - Orbital and millennial Antarctic climate variability over the past 800,000 years
AU - Jouzel, J.
AU - Masson-Delmotte, V.
AU - Cattani, O.
AU - Dreyfus, G.
AU - Falourd, S.
AU - Hoffmann, G.
AU - Minster, B.
AU - Nouet, J.
AU - Barnola, M.
AU - Chappellaz, J.
AU - Fischer, H.
AU - Gallet, J.C.
AU - Johnsen, Sigfus Johann
AU - Leuenberger, M.
AU - Loulergue, L.
AU - Luethi, D.
AU - Oerter, H.
AU - Parrenin, F.
AU - Raisbeck, G.
AU - Raynaud, D.
AU - Schilt, A.
AU - Schwander, J.
AU - Selmo, E.
AU - Souchez, R.
AU - Spahni, R.
AU - Stauffer, B.
AU - Steffensen, Jørgen Peder
AU - Stenni, B.
AU - Stocker, T.F.
AU - Tison, J.L.
AU - Werner, M.
AU - Wolff, E.W.
PY - 2007
Y1 - 2007
N2 - 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.
Udgivelsesdato: 10.08
AB - 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.
Udgivelsesdato: 10.08
U2 - 10.1126/science.1141038
DO - 10.1126/science.1141038
M3 - Journal article
VL - 317
SP - 793
EP - 796
JO - Science
JF - Science
SN - 0036-8075
IS - 5839
ER -
