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Characterization and Evaluation of Elevation Data Uncertainty in Water Resources Modeling with GIS

机译:基于GIS的水资源建模中高程数据不确定度的表征与评价。

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Grid based digital elevation models (DEM) are commonly used in water resources modeling. The quality of readily available DEM, however, varies from source to source in terms of horizontal resolution and vertical accuracy which are the two important aspects of elevation uncertainty in the modeling with raster GIS. This paper addresses the issue of elevation data uncertainty in GIS supported hydrologic simulations. The essential role of elevation data in the modeling is revealed by presenting DEM processing processes in distributed and semi-distributed hydrologic analyses. It is very difficult to examine the elevation uncertainties analytically due to complexities of the hydrologic models. An ideal approach is to assess the effect of the DEM uncertainty by applying varying resolutions or accuracies of elevation data in the modeling. Different grid sizes of DEM are used in observing DEM resolution dependence and resulting model outputs are compared to obtain a profile of its effect. Impact of DEM vertical accuracy is explored by Monte Carlo simulation with a large number of DEM realizations generated based on different levels of specified error. The approach is implemented in a case study with a topography based hydrologic model on an experimental watershed to analyze both aspects of the uncertainty. The results show that both DEM grid size and vertical accuracy could have profound effect on hydrologic modeling performance. The impact can be compensated by model calibrations due to interactions between model parameters and spatial factors. The study indicates that the DEM uncertainty can be effectively evaluated using the applied method. The work is to provide some insight into the characterization of elevation data quality and the association between topography and water resources models.
机译:基于网格的数字高程模型(DEM)通常用于水资源建模中。但是,在水平分辨率和垂直精度方面,随时可用的DEM的质量因来源而异,这是使用栅格GIS建模时高程不确定性的两个重要方面。本文解决了GIS支持的水文模拟中海拔数据不确定性的问题。通过在分布式和半分布式水文分析中介绍DEM处理过程,可以揭示高程数据在建模中的重要作用。由于水文模型的复杂性,很难以分析方式检查高程不确定性。一种理想的方法是通过在模型中应用不同的分辨率或高程数据的准确性来评估DEM不确定性的影响。 DEM的不同网格大小用于观察DEM分辨率依赖性,并且比较所得的模型输出以获得其效果的概况。通过蒙特卡洛模拟探索DEM垂直精度的影响,并根据不同级别的指定误差生成大量的DEM实现。在案例研究中使用基于地形的水文模型在实验分水岭上实施该方法,以分析不确定性的两个方面。结果表明,DEM网格尺寸和垂直精度都可能对水文建模性能产生深远影响。由于模型参数和空间因素之间的相互作用,可以通过模型校准来补偿影响。研究表明,使用所应用的方法可以有效地评估DEM不确定性。这项工作旨在对海拔数据质量的表征以及地形和水资源模型之间的关联提供一些见识。

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