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.


Science 31 October 1997:
Vol. 278. no. 5339, pp. 825 - 827
DOI: 10.1126/science.278.5339.825

Reports

The Holocene-Younger Dryas Transition Recorded at Summit, Greenland

K. C. Taylor, P. A. Mayewski, R. B. Alley, E. J. Brook, A. J. Gow, P. M. Grootes, D. A. Meese, E. S. Saltzman, J. P. Severinghaus, M. S. Twickler, J. W. C. White, S. Whitlow, G. A. Zielinski

Analysis of ice from Dye-3, Greenland, has demonstrated that the transition between the Younger Dryas and Holocene climate periods occurred over a 40-year period. A near annually resolved, multiparameter record of the transition recorded in the GISP2 core from Summit, Greenland, shows that most of the transition occurred in a series of steps with durations of about 5 years. Some climate proxies associated with mid-latitude sources appear to have changed about 15 years before climate proxies associated with more northern regions. Changes in atmospheric water vapor are likely to have played a large role in the climate transition.

K. C. Taylor, Desert Research Institute, University and Community College System of Nevada, Reno, NV 89506, USA.
P. A. Mayewski, M. S. Twickler, S. Whitlow, G. A. Zielinski, Climate Change Research Center, Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH 03824, USA.
R. B. Alley, Earth System Science Center, The Pennsylvania State University, University Park, PA 16802, USA.
E. J. Brook, Departments of Geology and Environmental Science, Washington State University, Vancouver, WA 98686, USA.
A. J. Gow and D. A. Meese, U.S. Army Cold Regions Research and Engineering Laboratory, Hanover, NH 03755, USA.
P. M. Grootes, C-14 Laboratory of the Christian Albrechts University Kiel, Leibnizstrasse 19, Kiel, Germany.
E. S. Saltzman, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL 33149, USA.
J. P. Severinghaus, Graduate School of Oceanography, University of Rhode Island, Kingston, RI 02819, USA.
J. W. C. White, INSTAAR and Department of Geological Sciences, University of Colorado, Boulder, CO 80309, USA.


Read the Full Text


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Recent changes in solar outputs and the global mean surface temperature. III. Analysis of contributions to global mean air surface temperature rise.
M. Lockwood (2008)
Proc R Soc A 464, 1387-1404
   Abstract »    Full Text »    PDF »
Unstable Younger Dryas climate in the northeast North Atlantic.
H. Ebbesen and M. Hald (2004)
Geology 32, 673-676
   Abstract »    Full Text »    PDF »
Global climate models: Past, present, and future.
M. Stute, A. Clement, and G. Lohmann (2001)
PNAS 98, 10529-10530
   Full Text »    PDF »
Ice-core evidence of abrupt climate changes.
R. B. Alley (2000)
PNAS 97, 1331-1334
   Abstract »    Full Text »    PDF »
Abrupt Climate Change at the End of the Last Glacial Period Inferred from Trapped Air in Polar Ice.
J. P. Severinghaus and E. J. Brook (1999)
Science 286, 930-934
   Abstract »    Full Text »
Genetics, archaeology, and Holocene hunter-gatherers.
J. F. O'Connell (1999)
PNAS 96, 10562-10563
   Full Text »    PDF »
Sudden climate transitions during the Quaternary.
J. Adams, M. Maslin, and E. Thomas (1999)
Progress in Physical Geography 23, 1-36
   Abstract »    PDF »
A calendar age estimate of the Younger Dryas-Holocene boundary at Krakenes, western Norway.
S. Gulliksen, H. H. Birks, G. Possnert, and J. Mangerud (1998)
The Holocene 8, 249-259
   Abstract »    PDF »



To Advertise     Find Products


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