Timing of Millennial-Scale Climate Change in Antarctica and Greenland During the Last Glacial Period

Author:

Blunier Thomas1,Brook Edward J.2

Affiliation:

1. Department of Geosciences, Guyot Hall, Princeton University, Princeton, NJ 08544, USA; Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland.

2. Department of Geology and Program in Environmental Science, Washington State University, 14204 Northeast Salmon Creek Avenue, Vancouver, WA 98686, USA.

Abstract

A precise relative chronology for Greenland and West Antarctic paleotemperature is extended to 90,000 years ago, based on correlation of atmospheric methane records from the Greenland Ice Sheet Project 2 and Byrd ice cores. Over this period, the onset of seven major millennial-scale warmings in Antarctica preceded the onset of Greenland warmings by 1500 to 3000 years. In general, Antarctic temperatures increased gradually while Greenland temperatures were decreasing or constant, and the termination of Antarctic warming was apparently coincident with the onset of rapid warming in Greenland. This pattern provides further evidence for the operation of a “bipolar see-saw” in air temperatures and an oceanic teleconnection between the hemispheres on millennial time scales.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference42 articles.

1. J. Schwander et al. J. Geophys. Res. 102 19483 (1997).

2. T. Blunier et al. Nature 394 739 (1998).

3. J. Jouzel et al. Clim. Dyn. 11 151 (1995).

4. E. J. Brook J. Severinghaus S. Harder M. Bender in Mechanisms of Millennial Scale Climate Change P. U. Clark R. S. Webb L. D. Keigwin Eds. [American Geophysical Union (AGU) Monograph AGU Washington DC 1999] vol. 112 pp. 165–175.

5. The choice of a reference time scale is not critical to our study because we are interested in the relative timing of Greenland and Antarctic temperature events. The GRIP and GISP2 ice cores were drilled 30 km apart on top of the Greenland ice sheet. They are equal in time resolution and core quality and the paleotemperature records are virtually identical on the time scales of interest here. All results are presented on the GISP2 Meese/Sowers time scale (6); see www.ngdc.noaa.gov/paleo/icecore/greenland/summit/document/notetime.htm for a description. However the same data set on the GRIP time scale can be found as supplemental information on Science Online (10) and at the National Oceanic and Atmospheric Administration (NOAA) Geophysical Data Center (www.ngdc.noaa.gov/paleo/paleo.html).

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