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首页> 外文期刊>Geoscientific Model Development >V2Karst V1.1: a parsimonious large-scale integrated vegetation–recharge model to simulate the impact of climate and land cover change in karst regions
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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 V1.1:一个简化的大规模综合植被补给模型,用于模拟气候和土地覆被变化对喀斯特地区的影响

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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:岩溶含水层是世界许多地区的重要饮用水来源。喀斯特地区具有高渗透性,可产生大量地下水,而地表径流通常可以忽略不计。结果,与其他渗透性较低的系统相比,这些系统中的补给对气候和土地覆盖变化的敏感性可能有所不同。然而,对于喀斯特地区气候和土地覆盖变化的综合影响知之甚少。特别是,在以前的喀斯特水文模型中,土地覆盖的表示及其对蒸散的控制非常有限。在这项研究中,我们通过以下方式解决了这一差距:(1)通过引入第一个大规模水文模型,其中包括对岩溶和土地覆盖特性的明确表示;(2)通过对模型的补给量生产进行深入分析行为。为了实现这些目标,我们用新模型(V2Karst V1.1)中的显式,机械和简约方法代替了以往的大型岩溶补给模型(VarKarst)的蒸散估算的经验方法。通过评估模型重现观测到的蒸散量和土壤水分模式的能力,并证明控制模型过程符合预期,我们证明了V2Karst模拟在四个碳酸盐岩FLUXNET站点上的可行性。使用合成输入数据进行的其他虚拟实验系统地研究了补给对降水特征(总量和时间分布)和土地覆盖特性的敏感性。这种方法证实了这些敏感性与期望相符,并提供了对未来变化的潜在影响的初步见解。 V2Karst是第一个能够研究大规模土地覆盖和气候变化对喀斯特地区地下水补给的联合影响的模型。

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