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High chance that current atmospheric greenhouse concentrations commit to warmings greater than 1.5?°C over land

机译:当前大气中温室气体的浓度很可能导致陆地上的变暖超过1.5?C

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The recent Paris UNFCCC climate meeting discussed the possibility of limiting global warming to 2?°C since pre-industrial times, or possibly even 1.5?°C, which would require major future emissions reductions. However, even if climate is stabilised at current atmospheric greenhouse gas (GHG) concentrations, those warming targets would almost certainly be surpassed in the context of mean temperature increases over land only. The reason for this is two-fold. First, current transient warming lags significantly below equilibrium or "committed" warming. Second, almost all climate models indicate warming rates over land are much higher than those for the oceans. We demonstrate this potential for high eventual temperatures over land, even for contemporary GHG levels, using a large set of climate models and for which climate sensitivities are known. Such additional land warming has implications for impacts on terrestrial ecosystems and human well-being. This suggests that even if massive and near-immediate emissions reductions occur such that atmospheric GHGs increase further by only small amounts, careful planning is needed by society to prepare for higher land temperatures in an eventual equilibrium climatic state.
机译:最近的巴黎《联合国气候变化框架公约》气候会议讨论了自工业化之前的时间将全球变暖限制在2?C或什至1.5?C的可能性,这将需要未来的大量减排。但是,即使将气候稳定在当前的大气温室气体(GHG)浓度下,仅在平均气温升高的情况下,几乎可以肯定会超过那些变暖目标。其原因有两个。首先,当前的瞬态变暖明显滞后于平衡变暖或“定型”变暖。其次,几乎所有的气候模型都表明陆地上的升温速率远高于海洋。我们使用大量的气候模型并且已知气候敏感性,证明了陆地上最终高温的潜力,甚至对于当代的温室气体排放水平也是如此。这种额外的土地变暖对陆地生态系统和人类福祉产生影响。这表明,即使发生大规模和近乎即时的排放减少,以致大气温室气体仅进一步少量增加,社会仍需要进行仔细的计划,以为最终处于平衡气候状态的更高的土地温度做准备。

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