Zanib Badar, Ishfaq Ahmad, Touqeer Ahmad, Ibrahim Mufrah Almanjahie
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引用次数: 0
Abstract
Drought is a complex, slowly evolving hazard governed by multiple interacting hydro-climatic factors, making it difficult to monitor, characterize, and predict. Conventional single-variable indices fail to capture the nonlinear, asymmetric dependence between precipitation and temperature—a limitation that is particularly critical in data-scarce, high-mountain catchments, where incomplete drought characterization undermines the reliability of early-warning systems. To address this, we propose a novel vine-copula-based Multivariate Drought Index (VMDI) that integrates the Standardized Precipitation Index (SPI), the Standardized Precipitation Evapotranspiration Index (SPEI), and the Standardized Precipitation Temperature Index (SPTI) within a flexible, station-adaptive dependence-modeling framework. VMDI’s key novelty lies in its station-adaptive canonical vine (C-vine) copula structure in which each index is first transformed into uniform pseudo-observations via rank-based empirical CDFs. Dependence is then decomposed into unconditional (Tree 1) and conditional (Tree 2) pair-copulas with SPTI as the root variable, capturing both direct interactions and joint behavior conditioned on SPTI. Copula families are selected locally via information criteria, and Kendall’s \(\varvec{\tau }\) values derived from the fitted vine structure yield physically consistent, station-specific index weights. Validated across six stations in the Upper Indus Basin (UIB), VMDI substantially outperforms benchmark indices for precipitation-driven drought signals, achieving agreement improvements of 15–30%, MAE reductions exceeding 50%, skill-score gains of 30–40%, F1-score improvements of 33–37%, and lower-tail dependence coefficients above 0.70, while maintaining low conditional entropy (CE \(\varvec{<} \varvec{0.99}\)). For evapotranspiration-related drought conditions, JSDI outperforms VMDI relative to SPEI by about 27–38%, with the greatest improvements observed at the glacier-influenced stations of Bunji and Gilgit. Overall, VMDI and JSDI offer a complementary and operationally robust framework for comprehensive drought monitoring across complex mountain catchments.
干旱是一种复杂的、缓慢演变的灾害,由多种相互作用的水文气候因素控制,因此很难监测、描述和预测。传统的单变量指数无法捕捉降水和温度之间的非线性、不对称依赖关系——这一限制在数据稀缺的高山流域尤为重要,在这些地区,不完整的干旱特征会破坏预警系统的可靠性。为了解决这个问题,我们提出了一种新的基于葡萄树的多元干旱指数(VMDI),该指数将标准化降水指数(SPI)、标准化降水蒸散指数(SPEI)和标准化降水温度指数(SPTI)集成在一个灵活的、站自适应的依赖模型框架中。VMDI的关键新颖之处在于其自适应的典型藤(c -藤)联结结构,其中每个指标首先通过基于秩的经验CDFs转换为统一的伪观测值。然后,以SPTI为根变量,将依赖关系分解为无条件(树1)和条件(树2)对联,捕获以SPTI为条件的直接相互作用和联合行为。Copula家族通过信息标准在本地选择,Kendall的\(\varvec{\tau }\)值来自拟合的藤结构,产生物理上一致的,特定于站点的指标权重。在印度河上游流域(UIB)的六个站点进行验证后,VMDI大大优于降水驱动干旱信号的基准指数,实现了15-30的一致性改进%, MAE reductions exceeding 50%, skill-score gains of 30–40%, F1-score improvements of 33–37%, and lower-tail dependence coefficients above 0.70, while maintaining low conditional entropy (CE \(\varvec{<} \varvec{0.99}\)). For evapotranspiration-related drought conditions, JSDI outperforms VMDI relative to SPEI by about 27–38%, with the greatest improvements observed at the glacier-influenced stations of Bunji and Gilgit. Overall, VMDI and JSDI offer a complementary and operationally robust framework for comprehensive drought monitoring across complex mountain catchments.
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