Boulton Chris A, Allison Lesley C, Lenton Timothy M
Earth System Science, College of Life and Environmental Sciences, Laver Building (Level 7), University of Exeter, Exeter EX4 4QE, UK.
Nat Commun. 2014 Dec 8;5:5752. doi: 10.1038/ncomms6752.
The Atlantic Meridional Overturning Circulation (AMOC) exhibits two stable states in models of varying complexity. Shifts between alternative AMOC states are thought to have played a role in past abrupt climate changes, but the proximity of the climate system to a threshold for future AMOC collapse is unknown. Generic early warning signals of critical slowing down before AMOC collapse have been found in climate models of low and intermediate complexity. Here we show that early warning signals of AMOC collapse are present in a fully coupled atmosphere-ocean general circulation model, subject to a freshwater hosing experiment. The statistical significance of signals of increasing lag-1 autocorrelation and variance vary with latitude. They give up to 250 years warning before AMOC collapse, after ~550 years of monitoring. Future work is needed to clarify suggested dynamical mechanisms driving critical slowing down as the AMOC collapse is approached.
在不同复杂程度的模型中,大西洋经向翻转环流(AMOC)呈现出两种稳定状态。人们认为,AMOC不同状态之间的转变在过去的突然气候变化中起到了一定作用,但气候系统距离未来AMOC崩溃阈值的接近程度尚不清楚。在低复杂度和中等复杂度的气候模型中,已经发现了AMOC崩溃前临界减缓的一般早期预警信号。在此,我们表明,在一个完全耦合的大气-海洋环流模型中,在进行淡水注入实验的情况下,存在AMOC崩溃的早期预警信号。滞后1自相关和方差增加信号的统计显著性随纬度而变化。在监测约550年后,它们在AMOC崩溃前给出长达250年的预警。随着接近AMOC崩溃,需要未来的工作来阐明所提出的驱动临界减缓的动力学机制。