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Distributed Error Propagation Analysis for Automatic Drainage Basin Delineation

机译:流域自动划分的分布误差传播分析。

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Delineation of drainage basins is a popular terrain analysis method for digital elevation model (DEM) data. Currently,a deterministic delineation method is available in a number of terrain analysis software applications. The method uses elevation data for defining flow directions for each elevation point of a DEM and then follows flow paths from a pour point to all upstream points. The influence ofa DEM error in the delineation process can be handled by replacing a single DEM D with the distribution of possible correct DEMs p(D). This uncertainty can be integrated into automatic delineation by using the Monte Carlo method,which uses realisations of DEMs drawn from p(D) to calculate probability maps for drainage basin delineations. The benefits of using Monte Carlo-based probability estimation in comparison with deterministic delineation are numerous. Firstly,the Monte Carlo method gives additional information by providing a clear 'probability band' for the catchment boundary,where the width of the band is dependent on local topography and the parameters of the DEM error model. In the extreme case,the band covers large areas around the drainage divide. Secondly,in some cases there exist two or more alternative boundaries that will become visible using the Monte Carlo method,whereas a deterministic approach is forced to pick only one of them. The number of samples required to accurately estimate the uncertainties in delineations is not clear,but according to earlier studies,estimation can require hundreds or thousands of samples. Our experiments on a single computer have shown that the use of the Monte Carlo method together with drainage basin delineation algorithms is a computationally demanding problem. In addition,the problem in current terrain analysis software applications is that they are not designed for large DEMs,which require distribution of the processed data and computations between multiple computers. In this paper,we improve existing drainage basin delineation methods for uncertain DEM data by improving and comparing distributed algorithms,used for computing probability maps of the delineations. We measure the performance and behavior of algorithms in different cases and compare the results of MPI (with spatial distribution of the data)and GRID (without spatial distribution) based implementations.
机译:流域划分是用于数字高程模型(DEM)数据的一种流行的地形分析方法。当前,确定性描绘方法可用于许多地形分析软件应用中。该方法使用高程数据为DEM的每个高程点定义流向,然后遵循从倾泻点到所有上游点的流路。可以通过用可能的正确DEM p(D)的分布替换单个DEM D来处理描述过程中DEM错误的影响。可以使用蒙特卡洛方法将该不确定性集成到自动轮廓中,该方法使用从p(D)提取的DEM的实现来计算流域轮廓的概率图。与确定性描述相比,使用基于蒙特卡洛的概率估计有很多好处。首先,蒙特卡洛方法通过为流域边界提供清晰的“概率带”来提供附加信息,其中带的宽度取决于局部地形和DEM误差模型的参数。在极端情况下,该频段覆盖了排水沟周围的大部分区域。其次,在某些情况下,存在两个或更多个替代边界,这些边界将使用蒙特卡洛方法变得可见,而确定性方法则只能选择其中之一。准确估计轮廓不确定性所需的样本数量尚不清楚,但根据早期研究,估计可能需要数百或数千个样本。我们在单台计算机上进行的实验表明,将蒙特卡洛方法与流域盆地描绘算法一起使用是一个计算量很大的问题。另外,当前地形分析软件应用程序中的问题在于它们不是为大型DEM设计的,而大型DEM需要在多台计算机之间分配已处理的数据和计算。本文通过改进和比较分布式算法,改进了现有流域对不确定DEM数据的划定方法,用于计算划定概率图。我们在不同情况下测量算法的性能和行为,并比较基于MPI(具有数据的空间分布)和GRID(无空间分布)的实现的结果。

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