Dakos Vasilis, Scheffer Marten, van Nes Egbert H, Brovkin Victor, Petoukhov Vladimir, Held Hermann
Department of Aquatic Ecology and Water Quality Management, Wageningen University, P.O. Box 47, 6700 AA, Wageningen, The Netherlands.
Proc Natl Acad Sci U S A. 2008 Sep 23;105(38):14308-12. doi: 10.1073/pnas.0802430105. Epub 2008 Sep 11.
In the Earth's history, periods of relatively stable climate have often been interrupted by sharp transitions to a contrasting state. One explanation for such events of abrupt change is that they happened when the earth system reached a critical tipping point. However, this remains hard to prove for events in the remote past, and it is even more difficult to predict if and when we might reach a tipping point for abrupt climate change in the future. Here, we analyze eight ancient abrupt climate shifts and show that they were all preceded by a characteristic slowing down of the fluctuations starting well before the actual shift. Such slowing down, measured as increased autocorrelation, can be mathematically shown to be a hallmark of tipping points. Therefore, our results imply independent empirical evidence for the idea that past abrupt shifts were associated with the passing of critical thresholds. Because the mechanism causing slowing down is fundamentally inherent to tipping points, it follows that our way to detect slowing down might be used as a universal early warning signal for upcoming catastrophic change. Because tipping points in ecosystems and other complex systems are notoriously hard to predict in other ways, this is a promising perspective.
在地球历史上,相对稳定的气候时期常常被向截然不同状态的急剧转变所打断。对于此类突变事件的一种解释是,它们发生在地球系统达到临界临界点之时。然而,对于遥远过去的事件而言,这一点仍难以证实,而且要预测我们未来是否以及何时会达到气候突变的临界点则更加困难。在此,我们分析了八次古代气候突变,结果表明,在实际转变之前很久,波动就开始出现特征性放缓。这种放缓,以自相关性增加来衡量,在数学上可证明是临界点的一个标志。因此,我们的结果为过去的突变与关键阈值的跨越相关这一观点提供了独立的实证证据。由于导致放缓的机制从根本上说是临界点所固有的,所以我们检测放缓的方法可能被用作即将发生的灾难性变化的通用早期预警信号。鉴于生态系统和其他复杂系统中的临界点以其他方式很难预测,这是一个很有前景的观点。