在全球数据集中分解沿岸地下水位动态变化

Annika Nolte, E. Haaf, B. Heudorfer, Steffen Bender, Jens Hartmann
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摘要

摘要。地下水位(GWL)动态是地下水系统与地球系统之间复杂相互作用的结果。本研究旨在找出共同的水文地质模式,并深入了解其背后的相似性及其与沿海地区地下水的地貌、气候和人为控制之间的联系。根据约 8000 个地下水水文图计算出的统计指标、使用聚类算法的模式识别、使用随机森林分类和 SHapley Additive exPlanations(SHAPs)等综合方法,确定了 GWL 动态及其控制的最显著方面。水文地质相似性由四个代表不同 GWL 动态模式的群组定义。这些群组在全球不同大洲和不同气候带均可观察到,但同时又因区域和地方而异,表明控制因素之间存在复杂的相互作用。我们确定了区分 GWL 动态的主要控制因素,但也证明了目前在大空间尺度上解释 GWL 动态的能力有限,这主要归因于解释数据的不确定性。最后,本研究为系统性和整体性的地下水监测和建模提供了指导,并促使我们在预测气候引起的 GWL 变化时考虑到 GWL 动态的不同方面,以及使用可解释的机器学习技术来处理 GWL 的复杂性--尤其是在潜在控制信息有限或需要验证的情况下。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Disentangling coastal groundwater level dynamics in a global dataset
Abstract. Groundwater level (GWL) dynamics result from a complex interplay between groundwater systems and the Earth system. This study aims to identify common hydrogeological patterns and to gain a deeper understanding of the underlying similarities and their link to physiographic, climatic, and anthropogenic controls of groundwater in coastal regions. The most striking aspects of GWL dynamics and their controls were identified through a combination of statistical metrics, calculated from about 8000 groundwater hydrographs, pattern recognition using clustering algorithms, classification using random forest, and SHapley Additive exPlanations (SHAPs). Hydrogeological similarity was defined by four clusters representing distinct patterns of GWL dynamics. These clusters can be observed globally across different continents and climate zones but simultaneously vary regionally and locally, suggesting a complicated interplay of controlling factors. The main controls differentiating GWL dynamics were identified, but we also provide evidence for the currently limited ability to explain GWL dynamics on large spatial scales, which we attribute mainly to uncertainties in the explanatory data. Finally, this study provides guidance for systematic and holistic groundwater monitoring and modeling and motivates a consideration of the different aspects of GWL dynamics, for example, when predicting climate-induced GWL changes, and the use of explainable machine learning techniques to deal with GWL complexity – especially when information on potential controls is limited or needs to be verified.
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