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Do time-variable tracers aid the evaluation of hydrological model structure? A multimodel approach

机译:时变示踪剂是否有助于评估水文模型结构?多模型方法

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摘要

In this paper we explore the use of time-variable tracer data as a complementary tool for model structure evaluation. We augment the modular rainfall-runoff modeling framework FUSE (Framework for Understanding Structural Errors) with the ability to track the age distribution of water in all model stores and fluxes. We therefore gain the novel ability to compare tracer/water age signatures measured in a catchment with those predicted using hydrological models built from components based on four existing popular models. Key modeling decisions available in FUSE are evaluated against streamflow tracer dynamics using weekly observations of tracer concentration which reflect the tracer transit time distribution (TTD). Model structure choice is shown to have a significant effect on simulated water age characteristics, even when simulated flow series are very similar. We show that for a Scottish case study catchment, careful selection of model structure enables good predictions of both streamflow and tracer dynamics. We then use FUSE as a hypothesis testing tool to understand how different model characterization of TTDs and mean transit times affect multicriteria model performance. We demonstrate the importance of time variation in TTDs in simulating water movement along fast flow pathways, and investigate sensitivity of the models to assumptions about our ability to sample fast, near-surface flow.
机译:在本文中,我们探索使用时变跟踪数据作为模型结构评估的补充工具。我们利用跟踪所有模型库和通量中水的年龄分布的能力来扩展模块化降雨-径流建模框架FUSE(理解结构误差的框架)。因此,我们获得了一种新颖的功能,可以将流域中测得的示踪剂/水龄特征与使用根据基于四个现有流行模型的组件构建的水文模型预测的特征进行比较。使用每周观察到的示踪剂浓度来反映流示踪剂的动态,以评估FUSE中可用的关键建模决策,该动态反映了示踪剂的通过时间分布(TTD)。结果表明,即使模拟流量序列非常相似,模型结构的选择也会对模拟水龄特征产生重大影响。我们表明,对于苏格兰的案例研究流域,仔细选择模型结构可以对流量和示踪剂动力学进行良好的预测。然后,我们将FUSE用作假设检验工具,以了解TTD的不同模型表征和平均运输时间如何影响多准则模型性能。我们证明了TTDs中时间变化在模拟沿快速流动路径的水运动中的重要性,并研究了模型对我们对快速近地表水采样能力的假设的敏感性。

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  • 来源
    《Water resources research》 |2012年第5期|p.W05501.1-W05501.18|共18页
  • 作者单位

    National Institute of Water and Atmospheric Research, PO Box 8602, Christchurch 8440, New Zealand;

    Northern Rivers Institute, School of Geosciences, University of Aberdeen, Aberdeen AB24 3UF, UK;

    National Center for Atmospheric Research, PO Box 3000, Boulder, CO 80307-3000, USA;

    Northern Rivers Institute, School of Geosciences, University of Aberdeen, Aberdeen AB24 3UF, UK;

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