Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial period

被引:814
|
作者
Blunier, T
Brook, EJ
机构
[1] Princeton Univ, Dept Geosci, Princeton, NJ 08544 USA
[2] Univ Bern, Inst Phys, CH-3012 Bern, Switzerland
[3] Washington State Univ, Dept Geol, Vancouver, WA 98686 USA
[4] Washington State Univ, Environm Sci Program, Vancouver, WA 98686 USA
关键词
D O I
10.1126/science.291.5501.109
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
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.
引用
收藏
页码:109 / 112
页数:4
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