Climate change research often focuses on trends in the mean and variance. However, analyses of palaeoclimatic and contemporary dynamics reveal that climate memory — as measured for instance by temporal autocorrelation — may also change substantially over time. Here, we show that elevated temporal autocorrelation in climatic variables should be expected to increase the chance of critical transitions in climate-sensitive systems with tipping points. We demonstrate that this prediction is consistent with evidence from forests, coral reefs, poverty traps, violent conflict and ice sheet instability. In each example, the duration of anomalous dry or warm events elevates chances of invoking a critical transition. Understanding the effects of climate variability thus requires research not only on variance, but also on climate memory.
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This work was carried out under the programme of the Netherlands Earth System Science Centre (NESSC), financially supported by the Ministry of Education, Culture, and Science (OCW) and received funding from the European Union’s Horizon 2020 research and innovation Programme under the Marie Sklodowska-Curie grant. We thank A. Staal for the fruitful discussions and all the recommendations for literature to include in our tropical forest example, and I. van de Leemput for her input on the coral reef model.
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van der Bolt, B., van Nes, E.H., Bathiany, S. et al. Climate reddening increases the chance of critical transitions. Nature Clim Change 8, 478–484 (2018). https://doi.org/10.1038/s41558-018-0160-7
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