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Adjusting Mitigation Pathways to Stabilize Climate at 1.5°C and 2.0°C Rise in Global Temperatures to Year 2300

机译:调整缓解途径,以稳定到2300年全球温度升高1.5°C和2.0°C的气候

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摘要

To avoid the most dangerous consequences of anthropogenic climate change, the Paris Agreement provides a clear and agreed climate mitigation target of stabilizing global surface warming to under 2.0°C above preindustrial, and preferably closer to 1.5°C. However, policy makers do not currently know exactly what carbon emissions pathways to follow to stabilize warming below these agreed targets, because there is large uncertainty in future temperature rise for any given pathway. This large uncertainty makes it difficult for a cautious policy maker to avoid either: (1) allowing warming to exceed the agreed target or (2) cutting global emissions more than is required to satisfy the agreed target, and their associated societal costs. This study presents a novel Adjusting Mitigation Pathway (AMP) approach to restrict future warming to policy‐driven targets, in which future emissions reductions are not fully determined now but respond to future surface warming each decade in a self‐adjusting manner. A large ensemble of Earth system model simulations, constrained by geological and historical observations of past climate change, demonstrates our self‐adjusting mitigation approach for a range of climate stabilization targets ranging from 1.5°C to 4.5°C, and generates AMP scenarios up to year 2300 for surface warming, carbon emissions, atmospheric CO 2 , global mean sea level, and surface ocean acidification. We find that lower 21st century warming targets will significantly reduce ocean acidification this century, and will avoid up to 4?m of sea‐level rise by year 2300 relative to a high‐end scenario.
机译:为避免人为气候变化带来的最危险后果,《巴黎协定》提供了一个明确和商定的缓解气候变化目标,即将全球表面变暖稳定在工业化之前的2.0°C以下,最好是接近1.5°C。但是,决策者目前尚不确切知道要遵循哪些碳排放途径将升温稳定在这些商定的目标以下,因为任何给定途径未来的升温都存在很大不确定性。这种巨大的不确定性使得谨慎的政策制定者很难避免:(1)允许变暖超过商定的目标,或者(2)削减超过实现商定目标所需的全球排放量以及相关的社会成本。这项研究提出了一种新颖的“调整减缓途径”(AMP)方法,将未来的变暖限制在政策驱动的目标之内,该方法目前尚未完全确定未来的减排量,而是以自调整的方式对未来十年的地面变暖做出反应。由过去气候变化的地质和历史观测所约束​​的大量地球系统模型模拟,展示了我们针对1.5°C至4.5°C范围内的一系列气候稳定目标的自调整缓解方法,并生成了高达AMP情景2300年是表面变暖,碳排放,大气CO 2,全球平均海平面和表面海洋酸化的一年。我们发现,较低的21世纪变暖目标将大大减少本世纪的海洋酸化,并且相对于高端情景,到2300年将避免高达4?m的海平面上升。

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