The Likelihood of Recent Record Warmth

被引:32
作者
Mann, Michael E. [1 ]
Rahmstorf, Stefan [2 ]
Steinman, Byron A. [3 ]
Tingley, Martin [1 ,4 ]
Miller, Sonya K. [1 ]
机构
[1] Penn State Univ, Dept Meteorol, 503 Walker Bldg, University Pk, PA 16802 USA
[2] Potsdam Inst Climate Impact Res, Earth Syst Anal, POB 60 12 03, D-14412 Potsdam, Germany
[3] Univ Minnesota, Large Lakes Observ, Dept Earth & Environm Sci, 2205 E 5th St RLB 205, Duluth, MN 55812 USA
[4] Penn State Univ, Dept Stat, 503 Walker Bldg, University Pk, PA 16802 USA
来源
SCIENTIFIC REPORTS | 2016年 / 6卷
关键词
PACIFIC;
D O I
10.1038/srep19831
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
2014 was nominally the warmest year on record for both the globe and northern hemisphere based on historical records spanning the past one and a half centuries(1,2). It was the latest in a recent run of record temperatures spanning the past decade and a half. Press accounts reported odds as low as one-in-650 million that the observed run of global temperature records would be expected to occur in the absence of human-caused global warming. Press reports notwithstanding, the question of how likely observed temperature records may have have been both with and without human influence is interesting in its own right. Here we attempt to address that question using a semi-empirical approach that combines the latest (CMIP5(3)) climate model simulations with observations of global and hemispheric mean temperature. We find that individual record years and the observed runs of record-setting temperatures were extremely unlikely to have occurred in the absence of human-caused climate change, though not nearly as unlikely as press reports have suggested. These same record temperatures were, by contrast, quite likely to have occurred in the presence of anthropogenic climate forcing.
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页数:7
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