Substantial Risk of 21st Century AMOC Tipping even under Moderate Climate Change

René M. van Westen, Elian Y. P. Vanderborght, Michael Kliphuis, Henk A. Dijkstra
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Abstract

The Atlantic Meridional Overturning Circulation (AMOC) is a key component of the climate system and considered to be a tipping element. There is still a large uncertainty on the critical global warming level at which the AMOC will start to collapse. Here we analyse targeted climate model simulations, together with observations, reanalysis products and a suite of state-of-the-art climate model results to reassess this critical global warming level. We find a critical threshold of +3C global mean surface temperature increase compared to pre-industrial with a lower bound of +2.2C (10%-Cl). Such global mean surface temperature anomalies are expected to be reached after 2050. This means that the AMOC is more likely than not (> 50%) to tip within the 21st century under a middle-of-the-road climate change scenario and very likely (> 90%) to tip under a high emissions scenario. The AMOC collapse induced cooling is shown to be offset by the regional warming over Northwestern Europe during the 21st century, but will still induce severe impacts on society.
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即使在中度气候变化的情况下,21 世纪 AMOC 倾覆的风险也很大
大西洋经向翻转环流(AMOC)是气候系统的一个关键组成部分,被认为是一个临界要素。全球变暖到什么临界水平,大西洋经向翻转环流就会开始崩溃,目前仍存在很大的不确定性。在此,我们分析了有针对性的气候模式模拟、观测数据、再分析产品和一套最先进的气候模式结果,以重新评估这一临界全球变暖水平。我们发现,与工业革命前相比,全球平均表面温度的临界值为+3℃,下限为+2.2℃(10%-Cl)。这种全球平均表面温度异常预计将在 2050 年后达到。这意味着,在中度气候变化情景下,AMOC 在 21 世纪更有可能(> 50%)发生坍缩,而在高排放情景下则非常有可能(> 90%)发生坍缩。在 21 世纪期间,西北欧上空的区域变暖将抵消 AMOC 崩溃引起的降温,但仍将对社会造成严重影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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