The Holocene-Younger Dryas Transition Recorded at Summit, Greenland-Reference-Cited by-同舟云学术

The Holocene-Younger Dryas Transition Recorded at Summit, Greenland

Published:1997-10-31 Issue:5339 Volume:278 Page:825-827
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Taylor K. C.¹²³⁴⁵,Mayewski P. A.¹²³⁴⁵,Alley R. B.¹²³⁴⁵,Brook E. J.¹²³⁴⁵,Gow A. J.¹²³⁴⁵,Grootes P. M.¹²³⁴⁵,Meese D. A.¹²³⁴⁵,Saltzman E. S.¹²³⁴⁵,Severinghaus J. P.¹²³⁴⁵,Twickler M. S.¹²³⁴⁵,White J. W. C.¹²³⁴⁵,Whitlow S.¹²³⁴⁵,Zielinski G. A.¹²³⁴⁵

Affiliation:

1. K. C. Taylor, Desert Research Institute, University and Community College System of Nevada, Reno, NV 89506, USA.

2. 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.

3. R. B. Alley, Earth System Science Center, The Pennsylvania State University, University Park, PA 16802, USA.

4. E. J. Brook, Departments of Geology and Environmental Science, Washington State University, Vancouver, WA 98686, USA.

5. A. J. Gow and D. A. Meese, U.S. Army Cold Regions Research and Engineering Laboratory, Hanover, NH 03755, USA.

Abstract

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.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference32 articles.

1. Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores

2. Johnsen S. J., et al., ibid. 359, 311 (1992).

3. K. C. Taylor et al. ibid. 366 549 (1993).

4. R. B. Alley et al. ibid. 362 527 (1993).

5. The Accumulation Record from the GISP2 Core as an Indicator of Climate Change Throughout the Holocene

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