The Standardized Precipitation Index (SPI) is a critical tool for monitoring drought conditions, typically relying on normalized accumulated precipitation. While longer historical records of precipitation yield more accurate parameter estimates of marginal distribution, they often reflect nonstationary influences such as anthropogenic climate change and multidecadal natural variability. Traditional approaches either overlook this nonstationarity or address it with quasi-stationary reference periods. This study introduces a novel nonstationary SPI framework that utilizes generalized additive models (GAMs) to flexibly model the spatiotemporal variability inherent in drought processes. GAMs are employed to estimate parameters of the Gamma distribution, while dual extreme tails flexible models are integrated to robustly capture the probabilistic risk of extreme drought events. Future drought and wet extremes events in terms of return levels are calculated using an extended generalized Pareto distribution, which offers flexibility in modeling the entire distribution of the data while bypassing the threshold selection step. Results demonstrate that the proposed nonstationary SPI model is both stable and capable of reproducing known nonstationary drought patterns, while also providing new insights into the evolving dynamics of drought. This approach represents a significant advancement in drought modeling under changing climatic conditions.
翻译:标准化降水指数(SPI)是监测干旱状况的关键工具,通常依赖于归一化累积降水量。虽然较长的降水历史记录能提供更准确的边缘分布参数估计,但这些记录常反映出非平稳性影响,如人为气候变化和数十年尺度的自然变异性。传统方法要么忽略这种非平稳性,要么采用准平稳参考期进行处理。本研究提出了一种新颖的非平稳SPI框架,利用广义可加模型(GAMs)灵活建模干旱过程固有的时空变异性。通过GAMs估计Gamma分布参数,并整合双极端尾柔性模型以稳健捕捉极端干旱事件的概率风险。采用扩展广义帕累托分布计算未来干旱与湿润极端事件的回归水平,该分布能灵活建模数据整体分布,同时规避阈值选择步骤。结果表明,所提出的非平稳SPI模型兼具稳定性,能够复现已知的非平稳干旱模式,并为干旱演变动态提供新见解。该方法代表了变化气候条件下干旱建模的重要进展。