🤖 AI Summary
Traditional early warning signals in climate time series are often compromised by noise, trends, and long-range dependence, leading to false positives or missed detections. This work proposes a flexible Bayesian framework that models time-varying autocorrelation and variance through a mixture of two fractional Gaussian noise processes, while incorporating a time-varying Hurst exponent to capture dynamic signatures preceding critical transitions. The approach effectively distinguishes genuine early warning signals from spurious ones, accommodates irregularly sampled data, and enables computationally efficient inference via integrated nested Laplace approximation (INLA). When applied to reconstructed indices of Atlantic multidecadal variability, the method successfully identifies significant early warning signals and concurrently rules out false alarms in records of Dansgaard–Oeschger events.
📝 Abstract
Detecting early warning signals in climatic time series is essential for anticipating critical transitions and tipping points. Common statistical indicators include increased variance and lag-one autocorrelation prior to bifurcation points. However, these indicators are sensitive to observational noise, long-term mean trends, and long-memory dependence, all of which are prevalent in climatic time series. Such effects can easily obscure genuine signals or generate spurious detections. To address these challenges, we employ a flexible Bayesian framework for modelling time-varying autocorrelation in long-range dependent time series, also accounting for time-varying variance. The approach uses a mixture of two fractional Gaussian noise processes with a time-dependent weight function to represent fractional Gaussian noise with a time-varying Hurst exponent. Inference is performed via integrated nested Laplace approximation, enabling joint estimation of mean trends and handling of irregularly sampled observations. The strengths and limitations of detecting changes in the autocorrelation is investigated in extensive simulations. Applied to real climatic data sets, we find evidence of early warning signals in a reconstructed Atlantic multidecadal variability index, while dismissing such signals for paleoclimate records spanning the Dansgaard-Oeschger events.