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Analysis of Impacts of Climate Change and Human Activities on Hydrological Drought: a Case Study in the Wei River Basin, China

机译:气候变化和人类活动对水文干旱的影响分析:以渭河流域为例

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AbstractClimate change and human activity are the two major drivers that can alter hydrological cycle processes and influence the characteristics of hydrological drought in river basins. The present study selects the Wei River Basin (WRB) as a case study region in which to assess the impacts of climate change and human activity on hydrological drought based on the Standardized Runoff Index (SRI) on different time scales. The Generalized Additive Models in Location, Scale and Shape (GAMLSS) are used to construct a time-dependent SRI (SRIvar) considering the non-stationarity of runoff series under changing environmental conditions. The results indicate that the SRIvaris more robust and reliable than the traditional SRI. We also determine that different driving factors can influence the hydrological drought evolution on different time scales. On shorter time scales, the effects of human activity on hydrological drought are stronger than those of climate change; on longer time scales, climate change is considered to be the dominant factor. The results presented in this study are beneficial for providing a reference for hydrological drought analysis by considering non-stationarity as well as investigating how hydrological drought responds to climate change and human activity on various time scales, thereby providing scientific information for drought forecasting and water resources management over different time scales under non-stationary conditions.
机译: Abstract 气候变化和人类活动是可以改变水文循环过程的两个主要驱动因素影响流域水文干旱的特征。本研究选择渭河流域(WRB)作为案例研究区域,在该区域中,根据不同时间尺度上的标准径流指数(SRI)评估气候变化和人类活动对水文干旱的影响。考虑到变化的环境条件下径流序列的非平稳性,采用位置,尺度和形状的广义加性模型(GAMLSS)来构建时间相关的SRI(SRI var )。结果表明,SRI var 比传统的SRI更加健壮和可靠。我们还确定了不同的驱动因素可以在不同的时间尺度上影响水文干旱的演变。在较短的时间尺度上,人类活动对水文干旱的影响要强于气候变化。在更长的时间范围内,气候变化被认为是主导因素。通过考虑非平稳性以及调查水文干旱如何在不同的时间尺度上响应气候变化和人类活动,本研究中提出的结果有益于为水文干旱分析提供参考,从而为干旱预测和水资源提供科学信息非平稳条件下不同时间尺度上的管理。

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