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A comparative assessment of rainfall-runoff modelling against regional flow duration curves for ungauged catchments

机译:降雨径流模型对未凝固集水区的区域流动持续时间曲线的比较评估

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Rainfall-runoff modelling has long been a special subject in hydrological sciences, but identifying behavioural parameters in ungauged catchments is still challenging. In this study, we comparatively evaluated the performance of the local calibration of a rainfall-runoff model against regional flow duration curves (FDCs), which is a seemingly alternative method of classical parameter regionalisation for ungauged catchments. We used a parsimonious rainfall-runoff model over 45 South Korean catchments under semi-humid climate. The calibration against regional FDCs was compared with the simple proximity-based parameter rgeionalisation. Results show that transferring behavioural parameters from gauged to ungauged catchments significantly outperformed the local calibration against regional FDCs due to the absence of flow timing information in the regional FDCs. The behavioural parameters gained from observed hydro-graphs were likely to contain intangible flow timing information affecting predictability in ungauged catchments. Additional constraining with the rising limb density appreciably improved the FDC calibrations, implying that flow signatures in temporal dimensions would supplement the FDCs. As an alternative approach in data-rich regions, we suggest calibrating a rainfall-runoff model against regionalised hydro-graphs to preserve flow timing information. We also suggest use of flow signatures that can supplement hydro-graphs for calibrating rainfall-runoff models in gauged and ungauged catchments.
机译:Rainfall-Runoff Modeling长期以来一直是水文科学的特殊主题,但识别未凝固的流域的行为参数仍然具有挑战性。在这项研究中,我们相对评价了降雨径流模型对区域流动持续时间曲线(FDC)的局部校准的性能,这是一个看似替代的未凝固集水区的参数区域化方法。我们在半潮湿气候下使用了45多个韩国集水区的灾区降雨模型。将针对区域FDCS的校准与基于简单的基于接近的参数突发化进行了比较。结果表明,由于区域FDC中没有流量时序信息,从测量到未凝固的集水区的行为参数显着优于局部校准。从观察到的水力图中获得的行为参数可能包含影响未凝固气囊中可预测性的无形流量信息。额外的限制与上升的肢体密度明显改善了FDC校准,这意味着在时间尺寸中的流动签名可以补充FDC。作为数据丰富地区的替代方法,我们建议校准针对区域化水力图的降雨径流模型,以保持流量时序信息。我们还建议使用能够补充水力图的流动签名,以便在测量和未凝固的集水区中校准降雨径流模型。

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