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Temperature increase of 21st century mitigation scenarios

机译:21世纪缓解情景的温度升高

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摘要

Estimates of 21st Century global-mean surface temperature increase have generally been based on scenarios that do not include climate policies. Newly developed multigas mitigation scenarios, based on a wide range of modeling approaches and socioeconomic assumptions, now allow the assessment of possible impacts of climate policies on projected warming ranges. This article assesses the atmospheric CO2 concentrations, radiative forcing, and temperature increase for these new scenarios using two reduced-complexity climate models. These scenarios result in temperature increase of 0.5–4.4°C over 1990 levels or 0.3–3.4°C less than the no-policy cases. The range results from differences in the assumed stringency of climate policy and uncertainty in our understanding of the climate system. Notably, an average minimum warming of ≈1.4°C (with a full range of 0.5–2.8°C) remains for even the most stringent stabilization scenarios analyzed here. This value is substantially above previously estimated committed warming based on climate system inertia alone. The results show that, although ambitious mitigation efforts can significantly reduce global warming, adaptation measures will be needed in addition to mitigation to reduce the impact of the residual warming.
机译:对21世纪全球平均表面温度升高的估算通常基于不包括气候政策的情景。基于广泛的建模方法和社会经济假设,最新开发的多气体缓解方案现在可以评估气候政策对预计变暖范围的可能影响。本文使用两个降低复杂性的气候模型评估了这些新情景的大气CO2浓度,辐射强迫和温度升高。这些情况导致温度比1990年的水平升高了0.5–4.4°C,或者比无政策的情况低了0.3–3.4°C。该范围是由于假定的气候政策严格性和我们对气候系统的理解存在不确定性而导致的。值得注意的是,即使是在此分析的最严格的稳定情景下,平均最低升温仍为≈1.4°C(整个范围为0.5-2.8°C)。该值大大高于仅基于气候系统惯性的先前估计的承诺变暖。结果表明,尽管雄心勃勃的减缓努力可以大大减少全球变暖,但除减缓气候变化外,还需要采取适应措施以减少残余变暖的影响。

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