800,000 Years of Abrupt Climate Variability

被引:299
|
作者
Barker, Stephen [1 ]
Knorr, Gregor [2 ]
Edwards, R. Lawrence [3 ]
Parrenin, Frederic [4 ,5 ,6 ]
Putnam, Aaron E. [7 ,8 ]
Skinner, Luke C. [9 ]
Wolff, Eric [10 ]
Ziegler, Martin [1 ]
机构
[1] Cardiff Univ, Sch Earth & Ocean Sci, Cardiff CF10 3AT, S Glam, Wales
[2] Alfred Wegener Inst, D-27570 Bremerhaven, Germany
[3] Univ Minnesota, Dept Earth Sci, Minneapolis, MN 55455 USA
[4] CNRS, Lab Glaciol, F-38400 Grenoble, France
[5] Univ Grenoble 1, F-38400 Grenoble, France
[6] Lab Chronoenvironm, F-25000 Besancon, France
[7] Univ Maine, Dept Earth Sci, Orono, ME 04469 USA
[8] Univ Maine, Climate Change Inst, Orono, ME 04469 USA
[9] Univ Cambridge, Godwin Lab Palaeoclimate Res, Dept Earth Sci, Cambridge CB2 3EQ, England
[10] British Antarctic Survey, Cambridge CB3 0ET, England
基金
英国自然环境研究理事会; 美国国家科学基金会;
关键词
MILLENNIAL-SCALE; PHASE-RELATIONSHIPS; ICE CORES; GREENLAND; RECORD; SEESAW; MODEL; OCEAN; DEEP; CH4;
D O I
10.1126/science.1203580
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
We constructed an 800,000-year synthetic record of Greenland climate variability based on the thermal bipolar seesaw model. Our Greenland analog reproduces much of the variability seen in the Greenland ice cores over the past 100,000 years. The synthetic record shows strong similarity with the absolutely dated speleothem record from China, allowing us to place ice core records within an absolute timeframe for the past 400,000 years. Hence, it provides both a stratigraphic reference and a conceptual basis for assessing the long-term evolution of millennial-scale variability and its potential role in climate change at longer time scales. Indeed, we provide evidence for a ubiquitous association between bipolar seesaw oscillations and glacial terminations throughout the Middle to Late Pleistocene.
引用
收藏
页码:347 / 351
页数:5
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