🤖 AI Summary
This study addresses the challenge of modeling post-rainfall soil moisture drying dynamics—characterized by multi-stage, non-stationary, scale-heterogeneous data and unknown prior parameters. We propose an adaptive Bayesian online change-point analysis framework featuring two key innovations: (1) particle-filter-based sequential Monte Carlo inference for real-time identification of piecewise drying behavior; and (2) an online learning mechanism incorporating stochastic gradient updates for continuous, adaptive estimation of core parameters such as drying rate. The method integrates Bayesian change-point detection, prior distribution modeling, and optimization-driven learning. Evaluated on synthetic data and multi-site field observations from Austria and the United States, it achieves accurate, site-specific quantification of drying rates and significantly outperforms static models. This framework establishes a new paradigm for real-time monitoring and adaptive modeling of soil hydrological processes.
📝 Abstract
Continuous soil-moisture measurements provide a direct lens on subsurface hydrological processes, notably the post-rainfall "drydown" phase. Because these records consist of distinct, segment-specific behaviours whose forms and scales vary over time, realistic inference demands a model that captures piecewise dynamics while accommodating parameters that are unknown a priori. Building on Bayesian Online Changepoint Detection (BOCPD), we introduce two complementary extensions: a particle-filter variant that substitutes exact marginalisation with sequential Monte Carlo to enable real-time inference when critical parameters cannot be integrated out analytically, and an online-gradient variant that embeds stochastic gradient updates within BOCPD to learn application-relevant parameters on the fly without prohibitive computational cost. After validating both algorithms on synthetic data that replicate the temporal structure of field observations-detailing hyperparameter choices, priors, and cost-saving strategies-we apply them to soil-moisture series from experimental sites in Austria and the United States, quantifying site-specific drydown rates and demonstrating the advantages of our adaptive framework over static models.