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Delayed emergence of a global temperature response after emission mitigation

机译:减排后全球温度响应的延迟出现

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A major step towards achieving the goals of the Paris agreement would be a measurable change in the evolution of global warming in response to mitigation of anthropogenic emissions. The inertia and internal variability of the climate system, however, will delay the emergence of a discernible?response even to strong, sustained mitigation. Here, we investigate when we could expect a significant change in the evolution of global mean surface temperature after strong mitigation of individual climate forcers. Anthropogenic CO 2 has the highest potential for a rapidly measurable influence, combined with long term benefits, but the required mitigation is very strong. Black Carbon (BC) mitigation could be rapidly discernible, but has a low net gain in the longer term. Methane mitigation combines rapid effects on surface temperature with long term effects. For other gases or aerosols, even fully removing anthropogenic emissions is unlikely to have a discernible impact before mid-century.
机译:实现巴黎协议目标的重大步骤将是全球变暖的演变变动,以应对人为排放的减轻。然而,气候系统的惯性和内部可变性将推迟出现可辨别的?响应甚至强烈,持续缓解。在这里,我们何时调查,当我们在强烈减轻个体气候侵略后,我们可以期望全球平均表面温度的演变发生重大变化。人为CO 2具有迅速可测量的影响的最高潜力,结合长期效益,但所需的缓解非常强。黑碳(BC)缓解可能会迅速辨别,但长期净收益低。甲烷缓解与长期效果相结合了对表面温度的快速影响。对于其他气体或气溶胶,甚至完全除去人为的排放不太可能在中世纪之前具有可辨别的影响。

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