A Reconstruction of Regional and Global Temperature for the Past 11,300 Years

被引:1311
作者
Marcott, Shaun A. [1 ]
Shakun, Jeremy D. [2 ]
Clark, Peter U. [1 ]
Mix, Alan C. [1 ]
机构
[1] Oregon State Univ, Coll Earth Ocean & Atmospher Sci, Corvallis, OR 97331 USA
[2] Harvard Univ, Dept Earth & Planetary Sci, Cambridge, MA 02138 USA
关键词
HIGH-RESOLUTION; CLIMATE-CHANGE; ASIAN MONSOON; HOLOCENE; CIRCULATION; RECORD; VALUES;
D O I
10.1126/science.1228026
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
Surface temperature reconstructions of the past 1500 years suggest that recent warming is unprecedented in that time. Here we provide a broader perspective by reconstructing regional and global temperature anomalies for the past 11,300 years from 73 globally distributed records. Early Holocene (10,000 to 5000 years ago) warmth is followed by similar to 0.7 degrees C cooling through the middle to late Holocene (<5000 years ago), culminating in the coolest temperatures of the Holocene during the Little Ice Age, about 200 years ago. This cooling is largely associated with similar to 2 degrees C change in the North Atlantic. Current global temperatures of the past decade have not yet exceeded peak interglacial values but are warmer than during similar to 75% of the Holocene temperature history. Intergovernmental Panel on Climate Change model projections for 2100 exceed the full distribution of Holocene temperature under all plausible greenhouse gas emission scenarios.
引用
收藏
页码:1198 / 1201
页数:4
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