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Representation of landscape variability and lateral redistribution processes for large-scale hydrological modelling in semi-arid areas

机译:半干旱地区大型水文模型的景观变异性和横向再分布过程的表示

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The spatial variability of landscape features such as topography, soils and vegetation defines the spatial pattern of hydrological state variables like soil moisture. Spatial variability thereby controls the functional behaviour of the landscape in terms of its runoff response. A consequence of spatial variability is that exchange processes between landscape patches can occur at various spatial scales ranging from the plot to the basin scale. In semi-arid areas, the lateral redistribution of surface runoff between adjacent landscape patches is an important process. For applications to large river basins of 10(4)-10(5) km(2) in size, a multi-scale landscape discretization scheme is presented in this paper. The landscape is sub-divided into modelling units within a hierarchy of spatial scale levels. By delineating areas characterized by a typical toposequence, organised and random variability of landscape characteristics is captured in the model. Using runoff-runon relationships with transition frequencies based on areal fractions of modelling units, lateral surface and subsurface water fluxes between modelling units at the hillslope scale are represented. Thus, the new approach allows for a manageable description of interactions between fine-scale landscape features for inclusion in coarse-scale models. Model applications for the State of Ceara (148,000 km(2)) in the north-east of Brazil demonstrate the importance of taking into account landscape variability and interactions between landscape patches in a semi-arid environment. Using mean landscape characteristics leads to a considerable underestimation of infiltration-excess surface runoff and total simulated runoff. Re-infiltration of surface runoff and lateral redistribution processes between landscape patches cause a reduction of runoff volumes at the basin scale and contribute to the amplification of variations in runoff volumes relative to variations in rainfall volumes for semi-arid areas. (C) 2004 Elsevier B.V. All rights reserved.
机译:景观特征(如地形,土壤和植被)的空间变异性定义了水文状态变量(如土壤湿度)的空间格局。因此,空间变异性根据径流响应来控制景观的功能行为。空间变异性的结果是,景观斑块之间的交换过程可能发生在从样地到盆地尺度的各种空间尺度上。在半干旱地区,相邻景观斑块之间的地表径流横向重新分布是一个重要过程。为了应用于大小为10(4)-10(5)km(2)的大型流域,本文提出了一种多尺度景观离散化方案。在空间比例级别的层次结构中,景观被细分为建模单元。通过描绘典型的典型地形特征,在模型中捕获了景观特征的有组织的和随机的变化。基于模型单元的面积分数,使用具有过渡频率的径流-径流关系,可以表示山坡尺度上模型单元之间的侧面和地下水通量。因此,新方法允许对包含在粗尺度模型中的细尺度景观特征之间的交互进行可管理的描述。巴西东北部塞阿拉州(148,000 km(2))的模型应用证明了考虑半干旱环境中景观变异性和景观斑块之间相互作用的重要性。使用平均景观特征会大大低估入渗过量的地表径流和总模拟径流。地表径流之间的地表径流重新渗透和景观斑块之间的侧向再分配过程导致流域尺度上的径流量减少,并且相对于半干旱地区的降雨量变化,径流量的变化有所增加。 (C)2004 Elsevier B.V.保留所有权利。

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