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Understanding hydrological flow paths in conceptual catchment models using uncertainty and sensitivity analysis

机译:使用不确定性和敏感性分析了解概念性集水模型中的水文流动路径

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摘要

Increasing pressures on water quality due to intensification of agriculture have raised demands for environmental modeling to accurately simulate the movement of diffuse (nonpoint) nutrients in catchments. As hydrological flows drive the movement and attenuation of nutrients, individual hydrological processes in models should be adequately represented for water quality simulations to be meaningful. In particular, the relative contribution of groundwater and surface runoff to rivers is of interest, as increasing nitrate concentrations are linked to higher groundwater discharges. These requirements for hydrological modeling of groundwater contribution to rivers initiated this assessment of internal flow path partitioning in conceptual hydrological models. In this study, a variance based sensitivity analysis method was used to investigate parameter sensitivities and flow partitioning of three conceptual hydrological models simulating 31 Irish catchments. We compared two established conceptual hydrological models (NAM and SMARG) and a new model (SMART), produced especially for water quality modelling. In addition to the criteria that assess streamflow simulations, a ratio of average groundwater contribution to total streamflow was calculated for all simulations over the 16 year study period. As observations time-series of groundwater contributions to streamflow are not available at catchment scale, the groundwater ratios were evaluated against average annual indices of base flow and deep groundwater flow for each catchment. The exploration of sensitivities of internal flow path partitioning was a specific focus to assist in evaluating model performances. Results highlight that model structure has a strong impact on simulated groundwater flow paths. Sensitivity to the internal pathways in the models are not reflected in the performance criteria results. This demonstrates that simulated groundwater contribution should be constrained by independent data to ensure results within realistic bounds if such models are to be used in the broader environmental sustainability decision making context.
机译:农业集约化对水质造成的压力越来越大,这就要求对环境模型进行准确模拟流域内分散(非点状)养分运动的环境建模的要求。由于水文流动驱动着养分的移动和衰减,因此模型中的各个水文过程应得到充分体现,以使水质模拟有意义。特别是,地下水和地表径流量对河流的相对贡献是令人关注的,因为硝酸盐浓度的增加与较高的地下水排放量有关。对地下水对河流的贡献进行水文模拟的这些要求开始了对概念性水文模型中内部流路划分的评估。在这项研究中,基于方差的敏感性分析方法用于研究模拟31个爱尔兰流域的三个概念性水文模型的参数敏感性和流量分配。我们比较了两个已建立的概念性水文模型(NAM和SMARG)和一个新模型(SMART),这些模型是专门为水质建模而制作的。除了评估流量模拟的标准外,还计算了16年研究期内所有模拟的平均地下水贡献与总流量之比。由于在集水区规模上没有观测到地下水对水流贡献的时间序列,因此对照每个集水区的基础流量和深层地下水流量的年平均指数评估了地下水比率。探索内部流路分配的敏感性是帮助评估模型性能的一个特定重点。结果表明,模型结构对模拟的地下水流路径有很大的影响。性能标准结果未反映对模型中内部途径的敏感性。这表明,如果要在更广泛的环境可持续性决策环境中使用此类模型,则应通过独立的数据来约束模拟的地下水贡献,以确保结果在现实的范围内。

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