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A methodology for preserving channel flow networks and connectivity patterns in large-scale distributed hydrological models

机译:在大规模分布式水文模型中保留河道网络和连通性模式的方法

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Physiographic data are often used to parameterize hydrological models and, in the past, physiographic parameters have often been derived manually. However, this can be a lengthy and unreliable process, particularly for application to a gridded hydrological or atmospheric model applied to large or continental-scale basins. An important attribute of gridded models is drainage direction. Current methods that determine drainage directions for large or continental-scale basins, by general circulation models (GCMs), route flow using lowest neighbour algorithms. These methods, however, do not reflect the hydrology of the basin subunit. This paper proposes a method of parameterizing hydrological models with physiographic data using the Arclnfo macro language to create an interface between the Topographic Parameterization (TOPAZ) software and the WATFLOOD hydrological model. The interface uses output raster data created by TOPAZ (i.e. drainage identification) to supply physiographic parameters required by WATFLOOD. The interface (WATPAZ) is an expert system based on a manual method of deriving parameters for the WATFLOOD distributed model. The WATPAZ interface uses grouped response units to subdivide the watershed. This allows large drainage basins to be subdivided at a scale that allows computational efficiency while preserving the hydrological variability of the watershed. To test whether the WATPAZ method improves the current GCM methodology for determining drainage directions, WATPAZ is applied on a local basin (Wolf Creek) a regional-scale basin, (Athabasca) and a continental-scale basin (Mackenzie). An examination of flow directions derived from this new method with current GCM methods is carried out. The results indicate that a substantial improvement is made to flow routing within the basin using the channel network to determine drainage directions for each segment.
机译:地物学数据通常用于参数化水文模型,并且过去,地物学参数通常是手动得出的。但是,这可能是一个漫长且不可靠的过程,特别是对于应用于网格化水文或大气模型的过程而言,该模型应用于大型或大陆性盆地。网格化模型的重要属性是排水方向。目前,通过通用环流模型(GCM)确定大型或大陆性盆地排水方向的方法是使用最低邻域算法来确定流量。但是,这些方法不能反映盆地亚单元的水文状况。本文提出了一种使用Arclnfo宏语言使用地貌数据对水文模型进行参数化的方法,以在地形参数化(TOPAZ)软件和WATFLOOD水文模型之间创建接口。该界面使用由TOPAZ创建的输出栅格数据(即排水识别)来提供WATFLOOD所需的生理参数。接口(WATPAZ)是基于手动方法为WATFLOOD分布式模型推导参数的专家系统。 WATPAZ接口使用分组的响应单位细分分水岭。这样可以将大型流域细分为一定规模,从而可以在保持流域水文变异性的同时提高计算效率。为了测试WATPAZ方法是否改进了当前用于确定排水方向的GCM方法,将WATPAZ应用于局部盆地(Wolf Creek),区域尺度盆地(Athabasca)和大陆尺度盆地(Mackenzie)。使用当前的GCM方法检查了从这种新方法得出的流向。结果表明,使用通道网络确定每个段的排水方向,可对流域内的水流路径进行重大改进。

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