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首页> 外文期刊>Hydrology and Earth System Sciences >HYPERstream: a multi-scale framework for streamflow routing in large-scale hydrological model
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HYPERstream: a multi-scale framework for streamflow routing in large-scale hydrological model

机译:HYPERstream:大型水文模型中用于水流路由的多尺度框架

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We present HYPERstream, an innovative streamflow routing scheme based on the width function instantaneous unit hydrograph (WFIUH) theory, which is specifically designed to facilitate coupling with weather forecasting and climate models. The proposed routing scheme preserves geomorphological dispersion of the river network when dealing with horizontal hydrological fluxes, irrespective of the computational grid size inherited from the overlaying climate model providing the meteorological forcing. This is achieved by simulating routing within the river network through suitable transfer functions obtained by applying the WFIUH theory to the desired level of detail. The underlying principle is similar to the block-effective dispersion employed in groundwater hydrology, with the transfer functions used to represent the effect on streamflow of morphological heterogeneity at scales smaller than the computational grid. Transfer functions are constructed for each grid cell with respect to the nodes of the network where streamflow is simulated, by taking advantage of the detailed morphological information contained in the digital elevation model (DEM) of the zone of interest. These characteristics make HYPERstream well suited for multi-scale applications, ranging from catchment up to continental scale, and to investigate extreme events (e.g., floods) that require an accurate description of routing through the river network. The routing scheme enjoys parsimony in the adopted parametrization and computational efficiency, leading to a dramatic reduction of the computational effort with respect to full-gridded models at comparable level of accuracy. HYPERstream is designed with a simple and flexible modular structure that allows for the selection of any rainfall-runoff model to be coupled with the routing scheme and the choice of different hillslope processes to be represented, and it makes the framework particularly suitable to massive parallelization, customization according to the specific user needs and preferences, and continuous development and improvements.
机译:我们介绍HYPERstream,这是一种基于宽度函数瞬​​时单位水位图(WFIUH)理论的创新性水流路由方案,该方案专门设计用于促进与天气预报和气候模型的耦合。所提出的路由方案在处理水平水文通量时可保留河网的地貌分布,而与从提供气象强迫的覆盖气候模型继承的计算网格大小无关。这是通过在适当的传递函数上模拟河流网络内的路由来实现的,该传递函数通过将WFIUH理论应用于所需的详细程度而获得。基本原理类似于在地下水水文学中采用的块有效分散,传递函数用来表示对形态非均质性流的影响,其规模小于计算网格。通过利用感兴趣区域的数字高程模型(DEM)中包含的详细形态信息,相对于模拟流量的网络节点为每个网格单元构造传递函数。这些特性使HYPERstream非常适合于从集水区到大陆范围的多尺度应用,并可用于调查需要准确描述通过河网路线的极端事件(例如洪水)。路由方案在采用的参数化和计算效率方面具有简约性,从而在相当精度的水平下,相对于全网格模型,大大减少了计算量。 HYPERstream采用简单灵活的模块化结构设计,允许选择任何降雨径流模型与路由方案结合,并选择要表示的不同坡度过程,这使得该框架特别适合大规模并行化,根据特定用户的需求和喜好进行定制,并不断发展和改进。

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