地下水流
虚假陈述
水循环
包气带
基岩
环境科学
空间异质性
生态水文学
水文学(农业)
水文模型
地质学
地下水
土壤科学
土壤水分
气候学
地貌学
岩土工程
政治学
生态系统
生物
法学
生态学
摘要
Subsurface heterogeneity is found across the whole hydrological cycle. It causes preferential flow in the soil, the vadose zone, and the bedrock. Aside of this, it has many other consequences for water flow and storage. This opinion paper discusses the implications of subsurface heterogeneity across the hydrological cycle and its implications for hydrological modeling. It focuses on the representation (and misrepresentation) of subsurface heterogeneity within hydrological models at different scales. Possible limitations to the prediction performance of hydrological models that disregard subsurface heterogeneity are introduced and discussed. The paper ends with practical recommendations to include subsurface heterogeneity into hydrological models, to parameterize them realistically, and to present possible directions for future research. WIREs Water 2016, 3:478–486. doi: 10.1002/wat2.1146 This article is categorized under: Science of Water > Hydrological Processes
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