基于可解释的机器学习,了解季节对低地下水期的影响

Andreas Wunsch, T. Liesch, N. Goldscheider
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摘要

摘要。众所周知,季节对地下水补给量有重大影响,因此对地下水水位也有重大影响;然而,其背后的关系却十分复杂,部分原因尚不清楚。本研究的目的是调查季节对地下水位(GWLs)的影响,尤其是在枯水期。为此,我们对来自德国 24 个地点的数据进行了人工神经网络训练。我们只将降水量和温度作为输入数据,并应用分层相关性传播来了解模型模拟地下水位的关系。我们发现,学习到的关系是可信的,因此与我们对主要物理过程的理解是一致的。我们的结果表明,在所调查的地点,模型学习到夏季是秋季全球降水量低值期的关键季节,而与前一个冬季的联系通常只是从属关系。具体来说,干燥的夏季对低水位期有很大影响,并产生(之前)潮湿的冬季无法弥补的缺水。因此,温度是夏季蒸散量的重要替代指标,通常被认为比降水更重要,尽管只是平均值。到目前为止,单次降水事件对 GWL 的影响最大,夏季降水似乎主要控制着秋季低 GWL 期的严重程度,而夏季较高的温度并不会系统地导致更严重的低水期。
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Towards understanding the influence of seasons on low-groundwater periods based on explainable machine learning
Abstract. Seasons are known to have a major influence on groundwater recharge and therefore groundwater levels; however, underlying relationships are complex and partly unknown. The goal of this study is to investigate the influence of the seasons on groundwater levels (GWLs), especially during low-water periods. For this purpose, we train artificial neural networks on data from 24 locations spread throughout Germany. We exclusively focus on precipitation and temperature as input data and apply layer-wise relevance propagation to understand the relationships learned by the models to simulate GWLs. We find that the learned relationships are plausible and thus consistent with our understanding of the major physical processes. Our results show that for the investigated locations, the models learn that summer is the key season for periods of low GWLs in fall, with a connection to the preceding winter usually only being subordinate. Specifically, dry summers exhibit a strong influence on low-water periods and generate a water deficit that (preceding) wet winters cannot compensate for. Temperature is thus an important proxy for evapotranspiration in summer and is generally identified as more important than precipitation, albeit only on average. Single precipitation events show by far the largest influences on GWLs, and summer precipitation seems to mainly control the severeness of low-GWL periods in fall, while higher summer temperatures do not systematically cause more severe low-water periods.
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