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Mapping dominant runoff processes: an evaluation of different approaches using similarity measures and synthetic runoff simulations

机译:绘制主要径流过程图:使用相似性测度和合成径流模拟对不同方法进行评估

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The identification of landscapes with similar hydrological behaviour is useful for runoff and flood predictions in small ungauged catchments. An established method for landscape classification is based on the concept of dominant runoff process (DRP). The various DRP-mapping approaches differ with respect to the time and data required for mapping. Manual approaches based on expert knowledge are reliable but time-consuming, whereas automatic GIS-based approaches are easier to implement but rely on simplifications which restrict their application range. To what extent these simplifications are applicable in other catchments is unclear. More information is also needed on how the different complexities of automatic DRP-mapping approaches affect hydrological simulations. brbr In this paper, three automatic approaches were used to map two catchments on the Swiss Plateau. The resulting maps were compared to reference maps obtained with manual mapping. Measures of agreement and association, a class comparison, and a deviation map were derived. The automatically derived DRP maps were used in synthetic runoff simulations with an adapted version of the PREVAH hydrological model, and simulation results compared with those from simulations using the reference maps. brbr The DRP maps derived with the automatic approach with highest complexity and data requirement were the most similar to the reference maps, while those derived with simplified approaches without original soil information differed significantly in terms of both extent and distribution of the DRPs. The runoff simulations derived from the simpler DRP maps were more uncertain due to inaccuracies in the input data and their coarse resolution, but problems were also linked with the use of topography as a proxy for the storage capacity of soils. brbr The perception of the intensity of the DRP classes also seems to vary among the different authors, and a standardised definition of DRPs is still lacking. Furthermore, we argue not to use expert knowledge for only model building and constraining, but also in the phase of landscape classification.
机译:识别具有相似水文行为的景观对于小型无流域的径流和洪水预报很有用。一种确定的景观分类方法是基于显性径流过程(DRP)的概念。各种DRP映射方法在映射所需的时间和数据方面有所不同。基于专家知识的手动方法可靠但耗时,而基于GIS的自动方法更易于实现,但依赖于简化方法,从而限制了其应用范围。这些简化措施在多大程度上适用于其他流域尚不清楚。还需要更多有关自动DRP映射方法的不同复杂性如何影响水文模拟的信息。 在本文中,使用三种自动方法绘制了瑞士高原上的两个流域的地图。将得到的地图与通过手动映射获得的参考地图进行比较。得出了一致性和关联性的度量,类比较和偏差图。自动导出的DRP图用于带有PREVAH水文模型改编版的合成径流模拟,并将模拟结果与使用参考图进行的模拟结果进行了比较。 用自动方法得出的具有最高复杂性和数据要求的DRP图谱与参考图谱最相似,而使用没有原始土壤信息的简化方法得出的DRP图谱在范围和分布上都存在很大差异。 DRP。由于输入数据的不准确及其粗略的分辨率,从更简单的DRP映射得出的径流模拟更加不确定,但是问题也与地形作为土壤存储能力的代名词有关。 不同作者之间对DRP类强度的理解似乎也有所不同,并且仍然缺乏对DRP的标准化定义。此外,我们主张不要将专家知识仅用于模型构建和约束,还应用于景观分类阶段。

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