Conditional Extremes with Graphical Models
Aiden Farrell, Emma F. Eastoe, Clement Lee
TL;DR
This work extends conditional multivariate extreme value analysis to data on graphs by introducing the MVAGG residual distribution and a structured, graphical CMEVM (SCMEVM). By combining asymmetric generalised Gaussian margins with a Gaussian copula and enforcing sparsity through graph-based precision matrices, the method accommodates both asymptotic independence and dependence, enabling accurate high-dimensional predictions and structure learning. A stepwise inference framework preserves information while dramatically improving scalability, and graphical structure learning via graphical lasso enables data-driven sparsity. Application to the upper Danube river basin demonstrates improved tail-dependence predictions and highlightsAI/AD mixtures that are not well captured by traditional AD-only models, indicating strong practical utility for risk assessment on river networks and similar infrastructures.
Abstract
Multivariate extreme value analysis quantifies the probability and magnitude of joint extreme events. River discharges from the upper Danube River basin provide a challenging dataset for such analysis because the data, which is measured on a spatial network, exhibits both asymptotic dependence and asymptotic independence. To account for both features, we extend the conditional multivariate extreme value model (CMEVM) with a new approach for the residual distribution. This allows sparse (graphical) dependence structures and fully parametric prediction. Our approach fills a current gap in statistical methodology by extending graphical extremes models to asymptotically independent random variables. Further, the model can be used to learn the graphical dependence structure when it is unknown a priori. To support inference in high dimensions, we propose a stepwise inference procedure that is computationally efficient and loses no information or predictive power. We show our method is flexible and accurately captures the extremal dependence for the upper Danube River basin discharges.
