Asynchrony of Antarctic and Greenland climate change during the last glacial period-Reference-Cited by-同舟云学术

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Asynchrony of Antarctic and Greenland climate change during the last glacial period

Published:1998-08 Issue:6695 Volume:394 Page:739-743
ISSN:0028-0836
Container-title:Nature
language:en
Short-container-title:Nature

Author:

Blunier T.,Chappellaz J.,Schwander J.,Dällenbach A.,Stauffer B.,Stocker T. F.,Raynaud D.,Jouzel J.,Clausen H. B.,Hammer C. U.,Johnsen S. J.

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/29447.pdf

Reference51 articles.

1. Dansgaard, W.et al. Evidence for general instability of past climate from a 250-kyr ice-core record. Nature 364, 218– 220 (1993).

2. Grootes, P. M., Stuiver, M., White, J. W. C., Johnsen, S. & Jouzel, J. Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores. Nature 366, 552–554 (1993).

3. Oeschger, H.et al. in Climate Processes and Climate Sensitivity(eds Hansen, J. E. & Takahashi, T.) 299–306 (Vol. 29, Geophys. Monogr. Ser., Am. Geophys. Union, Washington DC, (1984)).

4. Johnsen, S., Dahl-Jensen, D., Dansgaard, W. & Gundestrup, N. Greenland palaeotemperatures derived from GRIP bore hole temperature and ice core isotope profiles. Tellus B 47, 624– 629 (1995).

5. Schwander, J.et al. Age scale of the air in the summit ice: Implication for glacial–interglacial temperature change. J. Geophys. Res. 102, 19483–19494 (1997).

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