Characterisation of Groundwater Drought Using Distributed Modelling, Standardised Indices, and Principal Component Analysis.

IF 3.9 3区 环境科学与生态学 Q1 ENGINEERING, CIVIL
Water Resources Management Pub Date : 2025-01-01 Epub Date: 2024-11-08 DOI:10.1007/s11269-024-03997-4
V Christelis, M M Mansour, C R Jackson
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引用次数: 0

Abstract

A modelling framework was developed to characterise groundwater drought at a catchment scale in the absence of adequate observational records. The framework was used to characterise historical groundwater drought events for a Chalk aquifer in southern England over the period 1971-2004 during which three major drought events occurred. A numerical groundwater model was used to simulate the groundwater level fluctuations driven by historical time-variable and spatially non-uniform recharge inputs. The standardised groundwater level index (SGI) was applied to the simulated groundwater levels to evaluate the spatial pattern of groundwater drought and of their severity and duration. A dimensionality reduction method, namely principal component analysis (PCA), was applied to the SGI dataset and to the standardised precipitation index (SPI) to further explore the spatio-temporal drought characteristics. The analysis showed inconsistency in the spatial distribution of the duration and severity among the three studied events. PCA indicated that the SPI was not a good predictor of groundwater drought during the extreme European heatwave of 2003 whereas the proposed modelling framework correctly identified the resilience of the groundwater system to that event and in line with observations. Furthermore, significant differences were observed between the spatial patterns obtained from SPI and SGI datasets highlighting the important role that hydrological and hydrogeological features of a catchment have in groundwater drought development.

利用分布式模型、标准化指数和主成分分析表征地下水干旱。
在缺乏充分观测记录的情况下,开发了一个模型框架来描述集水区尺度上地下水干旱的特征。该框架被用于描述1971-2004年期间英格兰南部白垩含水层的历史地下水干旱事件,在此期间发生了三次主要干旱事件。采用数值地下水模型,模拟了历史时变和空间非均匀补给输入驱动下的地下水位波动。将标准化地下水位指数(SGI)应用于模拟地下水位,评价地下水干旱的空间格局及其严重程度和持续时间。将主成分分析(PCA)降维方法应用于SGI数据集和标准化降水指数(SPI),进一步探讨干旱的时空特征。分析表明,三种事件的持续时间和严重程度在空间分布上不一致。主成分分析表明,SPI不能很好地预测2003年欧洲极端热浪期间的地下水干旱,而所提出的建模框架正确地识别了地下水系统对该事件的恢复能力,并且与观测结果一致。此外,SPI和SGI数据获得的空间格局存在显著差异,突出了流域水文和水文地质特征在地下水干旱发展中的重要作用。
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来源期刊
Water Resources Management
Water Resources Management 环境科学-工程:土木
CiteScore
7.40
自引率
16.30%
发文量
332
审稿时长
9 months
期刊介绍: Water Resources Management is an international, multidisciplinary forum for the publication of original contributions and the exchange of knowledge and experience on the management of water resources. In particular, the journal publishes contributions on water resources assessment, development, conservation and control, emphasizing policies and strategies. Contributions examine planning and design of water resource systems, and operation, maintenance and administration of water resource systems. Coverage extends to these closely related topics: water demand and consumption; applied surface and groundwater hydrology; water management techniques; simulation and modelling of water resource systems; forecasting and control of quantity and quality of water; economic and social aspects of water use; legislation and water resources protection. Water Resources Management is supported scientifically by the European Water Resources Association, a scientific and technical nonprofit-making European association.
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