Uncertainty in predictions of the climate response to rising levels of greenhouse gases

被引:773
作者
Stainforth, DA
Aina, T
Christensen, C
Collins, M
Faull, N
Frame, DJ
Kettleborough, JA
Knight, S
Martin, A
Murphy, JM
Piani, C
Sexton, D
Smith, LA
Spicer, RA
Thorpe, AJ
Allen, MR
机构
[1] Univ Oxford, Dept Phys, Oxford OX1 3PU, England
[2] Univ Oxford, Comp Lab, Oxford OX1 3QD, England
[3] Hadley Ctr Climate Predict & Res, Met Off, Exeter EX1 3PB, Devon, England
[4] Rutherford Appleton Lab, Didcot OX11 0QX, Oxon, England
[5] Univ London London Sch Econ & Polit Sci, London WC2A 2AE, England
[6] Open Univ, Dept Earth Sci, Milton Keynes MK7 6AA, Bucks, England
[7] Univ Reading, Dept Meteorol, Reading RG6 6BB, Berks, England
基金
英国自然环境研究理事会;
关键词
D O I
10.1038/nature03301
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
The range of possibilities for future climate evolution(1-3) needs to be taken into account when planning climate change mitigation and adaptation strategies. This requires ensembles of multi-decadal simulations to assess both chaotic climate variability and model response uncertainty(4-9). Statistical estimates of model response uncertainty, based on observations of recent climate change(10-13), admit climate sensitivities - defined as the equilibrium response of global mean temperature to doubling levels of atmospheric carbon dioxide - substantially greater than 5 K. But such strong responses are not used in ranges for future climate change(14) because they have not been seen in general circulation models. Here we present results from the 'climateprediction.net' experiment, the first multi-thousand-member grand ensemble of simulations using a general circulation model and thereby explicitly resolving regional details(15-21). We find model versions as realistic as other state-of-the-art climate models but with climate sensitivities ranging from less than 2 K to more than 11 K. Models with such extreme sensitivities are critical for the study of the full range of possible responses of the climate system to rising greenhouse gas levels, and for assessing the risks associated with specific targets for stabilizing these levels.
引用
收藏
页码:403 / 406
页数:4
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