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A simple topography-driven and calibration-free runoff generation module

机译:简单的地形驱动和无需校准径流生成模块

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Reading landscapes and developing calibration-free runoff generation models that adequately reflect land surface heterogeneities remains the focus of much hydrological research. In this study, we report a novel and simple topography-driven runoff generation parameterization - the HAND-based Storage Capacity curve (HSC), which uses a topographic index (HAND, Height Above the Nearest Drainage) to identify hydrological similarity and the extent of saturated areas in catchments. The HSC can be used as a module in any conceptual rainfall-runoff model. Further, coupling the HSC parameterization with the mass curve technique (MCT) to estimate root zone storage capacity (S-uMax), we developed a calibration-free runoff generation module, HSC-MCT. The runoff generation modules of HBV and TOPMODEL were used for comparison purposes. The performance of these two modules (HSC and HSC-MCT) was first checked against the data-rich Bruntland Burn (BB) catchment in Scotland, which has a long time series of field-mapped saturation area extent. We found that HSC, HBV and TOPMODEL all perform well to reproduce the hydrograph, but the HSC module performs better in reproducing saturated area variation, in terms of correlation coefficient and spatial pattern. The HSC and HSC-MCT modules were subsequently tested for 323 MOPEX catchments in the US, with diverse climate, soil, vegetation and geological characteristics. In comparison with HBV and TOPMODEL, the HSC performs better in both calibration and validation, particularly in the catchments with gentle topography, less forest cover, and arid climate. Despite having no calibrated parameters, the HSC-MCT module performed comparably well with calibrated modules, highlighting the robustness of the HSC parameterization to describe the spatial distribution of the root zone storage capacity and the efficiency of the MCT method to estimate S-uMax. This novel and calibration-free runoff generation module helps to improve the prediction in ungauged
机译:阅读景观和开发无校准的径流发电模型,可充分反映土地表面异质性仍然是多种水文研究的重点。在这项研究中,我们报告了一种新颖的和简单的地形驱动的径流生成参数化 - 基于手基的存储容量曲线(HSC),它使用地形索引(手,高于最近的排水高度)来识别水文相似性和程度集水区的饱和区域。 HSC可以用作任何概念降雨径流模型中的模块。此外,将HSC参数化与质量曲线技术(MCT)耦合到估计根区存储容量(S-UMAX),我们开发了一种无校准的径流生成模块HSC-MCT。 HBV和TOPMODEL的径流生成模块用于比较目的。本两个模块(HSC和HSC-MCT)的性能首先检查苏格兰的数据丰富的Bruntland Burn(BB)集水区,该集水区具有长时间的现场映射饱和区。我们发现HSC,HBV和TOPMODEL都表现良好以再现水文,但是在相关系数和空间模式方面,HSC模块在再现饱和区域变化方面更好地执行。随后在美国测试了HSC和HSC-MCT模块323毫安集水区,具有多种的气候,土壤,植被和地质特征。与HBV和TOPMODEL相比,HSC在校准和验证方面更好地表现出更好的,特别是在具有柔和地形,较少的森林覆盖和干旱气候的集水区中。尽管没有校准参数,但HSC-MCT模块与校准模块相对良好地执行,突出显示HSC参数化的鲁棒性,以描述根区存储容量的空间分布和MCT方法估算S-UMAX的效率。这种新颖和无校准的径流产生模块有助于改善未凝固的预测

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