Warming caused by cumulative carbon emissions towards the trillionth tonne

被引:0
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作者
Myles R. Allen
David J. Frame
Chris Huntingford
Chris D. Jones
Jason A. Lowe
Malte Meinshausen
Nicolai Meinshausen
机构
[1] University of Oxford,Department of Physics
[2] OX1 3PU,Department of Meteorology
[3] UK,Department of Statistics
[4] Smith School of Enterprise and the Environment,undefined
[5] University of Oxford,undefined
[6] OX1 2BQ,undefined
[7] UK ,undefined
[8] Centre for Ecology and Hydrology,undefined
[9] Wallingford,undefined
[10] OX10 8BB,undefined
[11] UK ,undefined
[12] Met Office Hadley Centre,undefined
[13] FitzRoy Road,undefined
[14] Exeter,undefined
[15] EX1 3PB,undefined
[16] UK ,undefined
[17] Met Office Hadley Centre (Reading Unit),undefined
[18] University of Reading,undefined
[19] RG6 6BB,undefined
[20] Reading,undefined
[21] UK,undefined
[22] Potsdam Institute for Climate Impact Research,undefined
[23] University of Oxford,undefined
[24] OX1 3TG,undefined
[25] UK,undefined
来源
Nature | 2009年 / 458卷
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摘要
How quickly greenhouse-gas emissions need to be reduced in order to avoid what has been termed dangerous climate change is of fundamental importance. Two papers in this issue tackle the question from different standpoints, yet come to broadly similar conclusions. Meinshausen et al. relate the cumulative emission of greenhouse gasses by 2050 to the probability of exceeding the 2 °C of global warming above pre-industrial temperatures adopted by more than 100 countries as the threshold of dangerous climate change. They find that only about a third of economically recoverable oil, gas and coal reserves can be burned if global warming of 2 °C is to be avoided by 2100, an amount of fossil fuel that would be burned by 2029 if consumption remains at today's levels. Allen et al. use a combined climate and carbon cycle model to produce simulations spanning a range of climate futures consistent with the changes already observed. The 500 billionth tonne of anthropogenic carbon since 1750 was recently released into the atmosphere, and Allen et al. find that releasing a trillion tonnes of carbon in total is likely to cause a peak warming exceeding the 'acceptable' 2 °C temperature increase. Every tonne released thereafter increases the committed maximum warming in a predictable way, regardless of when it is released. Any effective climate mitigation regime must therefore achieve a cap on cumulative carbon dioxide emissions — one trillion tonnes would be a possible though optimistic target. In News and Views, Gavin Schmidt and David Archer consider these papers and other recent work focusing on establishing achievable emissions targets.
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页码:1163 / 1166
页数:3
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