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Allowable CO2 concentrations under the United Nations Framework Convention on Climate Change as a function of the climate sensitivity probability distribution function

机译:《联合国气候变化框架公约》下允许的二氧化碳浓度与气候敏感性概率分布函数的关系

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Article 2 of the United Nations Framework Convention on Climate Change (UNFCCC) calls for stabilization of greenhouse gas (GHG) concentrations at levels that prevent dangerous anthropogenic interference (DAI) in the climate system. Until recently, the consensus viewpoint was that the climate sensitivity (the global mean equilibrium warming for a doubling of atmospheric CO2 concentration) was 'likely' to fall between 1.5 and 4.5?K. However, a number of recent studies have generated probability distribution functions (pdfs) for climate sensitivity with the 95th percentile of the expected climate sensitivity as large as 10?K, while some studies suggest that the climate sensitivity is likely to fall in the lower half of the long-standing 1.5–4.5?K range. This paper examines the allowable CO2 concentration as a function of the 95th percentile of the climate sensitivity pdf (ranging from 2 to 8?K) and for the following additional assumptions: (i) the 50th percentile for the pdf of the minimum sustained global mean warming that causes unacceptable harm equal to 1.5 or 2.5?K; and (ii) 1%, 5% or 10% allowable risks of unacceptable harm. For a 1% risk tolerance and the more stringent harm-threshold pdf, the allowable CO2 concentration ranges from 323 to 268?ppmv as the 95th percentile of the climate sensitivity pdf increases from 2 to 8?K, while for a 10% risk tolerance and the less stringent harm-threshold pdf, the allowable CO2 concentration ranges from 531 to 305?ppmv. In both cases it is assumed that non-CO2 GHG radiative forcing can be reduced to half of its present value, otherwise; the allowable CO2 concentration is even smaller. Accounting for the fact that the CO2 concentration will gradually fall if emissions are reduced to zero, and that peak realized warming will then be less than the peak equilibrium warming (related to peak radiative forcing) allows the CO2 concentration to peak at 10–40?ppmv higher than the limiting values given above for a climate sensitivity 95th percentile at 4.5?K. Even allowing for the difference between peak realized and peak equilibrium warming, and assuming that present non-CO2 GHG forcing can be cut in half, a CO2 concentration of 410?ppmv or less constitutes DAI for every combination of harm-threshold pdf and risk tolerance considered here if the 95th percentile of the climate sensitivity pdf is 4.5?K or greater.
机译:《联合国气候变化框架公约》(UNFCCC)第2条要求将温室气体(GHG)浓度稳定在防止气候系统中危险的人为干扰(DAI)的水平。直到最近,共识观点还是认为气候敏感性(全球平均平衡变暖使大气中的CO2浓度增加一倍)“可能”落在1.5至4.5?K之间。但是,最近的一些研究已经生成了气候敏感性的概率分布函数(pdfs),预期气候敏感性的第95个百分位数高达10?K,而一些研究表明,气候敏感性可能下降到下半部分长期存在的1.5–4.5?K范围。本文研究了允许的CO2浓度与气候敏感性pdf的第95个百分位数(范围从2至8?K)和以下附加假设的关系:(i)最小持续全球平均值pdf的第50个百分位数导致无法接受的等于1.5或2.5?K伤害的变暖; (ii)造成不可接受伤害的1%,5%或10%允许风险。对于1%的风险容忍度和更严格的伤害阈值pdf,随着气候敏感性pdf的95%百分数从2增加到8?K,允许的CO2浓度范围为323至268?ppmv,而对于10%的风险容忍度危害阈值pdf不太严格,允许的CO2浓度范围为531至305?ppmv。在这两种情况下,都可以将非CO2温室气体的辐射强迫降低到其现值的一半,否则;允许的二氧化碳浓度甚至更小。考虑到以下事实:如果将排放量减少到零,CO2浓度将逐渐下降,然后峰值实现的变暖将小于峰值平衡变暖(与峰值辐射强迫有关),从而使CO2浓度在10–40达到峰值? ppmv高于上面给出的气候敏感性第95个百分位数在4.5?K时的极限值。即使考虑到峰值实现与峰值平衡变暖之间的差异,并假设可以将目前的非CO2温室气体强迫减少一半,对于伤害阈值pdf和风险承受能力的每种组合,CO2浓度为410?ppmvv或更少构成DAI如果气候敏感性pdf的第95个百分位数为4.5?K或更高,请在此处考虑。

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