The upper end of climate model temperature projections is inconsistent with past warming

被引:40
作者
Stott, Peter [1 ]
Good, Peter [1 ]
Jones, Gareth [1 ]
Gillett, Nathan [2 ]
Hawkins, Ed [3 ]
机构
[1] Met Off Hadley Ctr, Exeter EX1 3PB, Devon, England
[2] Environm Canada, Canadian Ctr Climate Modelling & Anal, Victoria, BC, Canada
[3] Univ Reading, NCAS Climate, Dept Meteorol, Reading RG6 6BB, Berks, England
来源
ENVIRONMENTAL RESEARCH LETTERS | 2013年 / 8卷 / 01期
基金
美国海洋和大气管理局;
关键词
climate change; detection and attribution; climate prediction; climate variability; PREDICTIONS; UNCERTAINTY;
D O I
10.1088/1748-9326/8/1/014024
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Climate models predict a large range of possible future temperatures for a particular scenario of future emissions of greenhouse gases and other anthropogenic forcings of climate. Given that further warming in coming decades could threaten increasing risks of climatic disruption, it is important to determine whether model projections are consistent with temperature changes already observed. This can be achieved by quantifying the extent to which increases in well mixed greenhouse gases and changes in other anthropogenic and natural forcings have already altered temperature patterns around the globe. Here, for the first time, we combine multiple climate models into a single synthesized estimate of future warming rates consistent with past temperature changes. We show that the observed evolution of near-surface temperatures appears to indicate lower ranges (5-95%) for warming (0.35-0.82 K and 0.45-0.93 K by the 2020s (2020-9) relative to 1986-2005 under the RCP4.5 and 8.5 scenarios respectively) than the equivalent ranges projected by the CMIP5 climate models (0.48-1.00 K and 0.51-1.16 K respectively). Our results indicate that for each RCP the upper end of the range of CMIP5 climate model projections is inconsistent with past warming.
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页数:8
相关论文
共 29 条
[1]   Quantifying the uncertainty in forecasts of anthropogenic climate change [J].
Allen, MR ;
Stott, PA ;
Mitchell, JFB ;
Schnur, R ;
Delworth, TL .
NATURE, 2000, 407 (6804) :617-620
[2]   Estimating signal amplitudes in optimal fingerprinting, part I: theory [J].
Allen, MR ;
Stott, PA .
CLIMATE DYNAMICS, 2003, 21 (5-6) :477-491
[3]   Checking for model consistency in optimal fingerprinting [J].
Allen, MR ;
Tett, SFB .
CLIMATE DYNAMICS, 1999, 15 (06) :419-434
[4]  
[Anonymous], 2007, CLIMATE CHANGE PHYS
[5]  
[Anonymous], 2007, Intergovernmental Panel on Climate Change [Core Writing Team IPCC, DOI DOI 10.1256/004316502320517344
[6]   Asymmetries in tropical rainfall and circulation patterns in idealised CO2 removal experiments [J].
Chadwick, Robin ;
Wu, Peili ;
Good, Peter ;
Andrews, Timothy .
CLIMATE DYNAMICS, 2013, 40 (1-2) :295-316
[7]   Aerosol contribution to the rapid warming of near-term climate under RCP 2.6 [J].
Chalmers, N. ;
Highwood, E. J. ;
Hawkins, E. ;
Sutton, R. ;
Wilcox, L. J. .
GEOPHYSICAL RESEARCH LETTERS, 2012, 39
[8]   Climate forcings and climate sensitivities diagnosed from coupled climate model integrations [J].
Forster, Piers M. de F. ;
Taylor, Karl E. .
JOURNAL OF CLIMATE, 2006, 19 (23) :6181-6194
[9]   Alternatives to stabilization scenarios [J].
Frame, D. J. ;
Stone, D. A. ;
Stott, P. A. ;
Allen, M. R. .
GEOPHYSICAL RESEARCH LETTERS, 2006, 33 (14)
[10]   Improved constraints on 21st-century warming derived using 160 years of temperature observations [J].
Gillett, N. P. ;
Arora, V. K. ;
Flato, G. M. ;
Scinocca, J. F. ;
von Salzen, K. .
GEOPHYSICAL RESEARCH LETTERS, 2012, 39