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V2Karst V1.1: a parsimonious large-scale integrated vegetation–recharge model to simulate the impact of climate and land cover change in karst regions

机译:V2KARST v1.1:一种典型的大型综合植被 - 充值模型,用于模拟气候和土地覆盖变化在喀斯特地区的影响

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Karst aquifers are an important source of drinking water in many regions of the world. Karst areas are highly permeable and produce large amounts of groundwater recharge, while surface runoff is often negligible. As a result, recharge in these systems may have a different sensitivity to climate and land cover changes than in other less permeable systems. However, little is known about the combined impact of climate and land cover changes in karst areas at large scales. In particular, the representation of land cover, and its controls on evapotranspiration, has been very limited in previous karst hydrological models. In this study, we address this gap (1)?by introducing the first large-scale hydrological model including an explicit representation of both karst and land cover properties, and (2)?by providing an in-depth analysis of the model's recharge production behaviour. To achieve these aims, we replace the empirical approach to evapotranspiration estimation of a previous large-scale karst recharge model (VarKarst) with an explicit, mechanistic and parsimonious approach in the new model (V2Karst V1.1). We demonstrate the plausibility of V2Karst simulations at four carbonate rock FLUXNET sites by assessing the model's ability to reproduce observed evapotranspiration and soil moisture patterns and by showing that the controlling modelled processes are in line with expectations. Additional virtual experiments with synthetic input data systematically explore the sensitivities of recharge to precipitation characteristics (overall amount and temporal distribution) and land cover properties. This approach confirms that these sensitivities agree with expectations and provides first insights into the potential impacts of future change. V2Karst is the first model that enables the study of the joint impacts of large-scale land cover and climate changes on groundwater recharge in karst regions.
机译:喀斯特含水层是世界许多地区的饮用水的重要来源。岩溶区域高度渗透性,产生大量地下水充电,而表面径流通常可以忽略不计。结果,这些系统中的充电可能对气候和陆地覆盖的改变具有比在其他更少的透水系统中的不同敏感性。然而,关于气候和土地覆盖变化在大尺度的喀斯特地区的综合影响几乎是知之甚少。特别是,陆地覆盖的代表及其对蒸散的对照,在以前的喀斯特水文模型中已经非常有限。在这项研究中,我们解决了这个差距(1)?通过引入第一个大规模水文模型,包括喀斯特和陆地覆盖物业的明确表示,(2)?通过提供对模型的充电生产进行深入分析行为。为实现这些目标,我们用新模型(V2KARST v1.1)中的明确,机械和解析方法取代了先前大型岩溶充电模型(Varkarst)的实证方法来取代了蒸发蒸发估计。我们通过评估模型再现观察到的蒸散和土壤水分模式的能力,证明了四个碳酸盐岩浮雕网站的V2KARST模拟的合理性,并通过表明控制建模的过程符合预期的能力。具有合成输入数据的附加虚拟实验系统地探索了降水特性(总体量和时间分配)和陆地覆盖特性的敏感性。这种方法证实,这些敏感性同意期望,并提供对未来变革的潜在影响的首要见解。 V2KARST是第一种型号,可以研究大型陆地覆盖和气候变化对喀斯特地区地下水充电的关节影响。

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