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A DEM-based approach for large-scale floodplain mapping in ungauged watersheds

机译:一个基于DEM的大规模泛洪叶映射方法在未凝固的流域中

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摘要

Binary threshold classifiers are a simple form of supervised classification methods that can be used in floodplain mapping. In these methods, a given watershed is examined as a grid of cells with a particular morphologic value. A reference map is a grid of cells labeled as flood and non-flood from hydraulic modeling or remote sensing observations. By using the reference map, a threshold on morphologic feature is determined to label the unknown cells as flood and non-flood (binary classification). The main limitation of these methods is the threshold transferability assumption in which a homogenous geomorphological and hydrological behavior is assumed for the entire region and the same threshold derived from the reference map (training area) is used for other locations (ungauged watersheds) inside the study area. In order to overcome this limitation and consider the threshold variability inside a large region, regression modeling is used in this paper to predict the threshold by relating it to the watershed characteristics. Application of this approach for North Carolina shows that the threshold is related to main stream slope, average watershed elevation, and average watershed slope. By using the Fitness (F) and Correct (C) criteria of C > 0.9 and F > 0.6, results show the threshold prediction and the corresponding floodplain for 100-year design flow are comparable to that from Federal Emergency Management Agency's (FEMA) Flood Insurance Rate Maps (FIRMs) in the region. However, the floodplains from the proposed model are underpredicted and overpredicted in the flat (average watershed slope <1%) and mountainous regions (average watershed slope >20%). Overall, the proposed approach provides an alternative way of mapping floodplain in data-scarce regions. (C) 2017 Elsevier B.V. All rights reserved.
机译:二进制阈值分类器是一种简单的监督分类方法,可用于洪泛区映射。在这些方法中,将给定的流域被检查为具有特定形态值的细胞网格。参考图是标记为洪水和来自液压建模或遥感观察的洪水的电池网格。通过使用参考图,确定形态学特征的阈值标记为洪水和非洪水(二进制分类)标记未知的小区。这些方法的主要限制是阈值可转移性假设,其中假设整个区域的均匀地貌和水文行为,并且从参考图(训练区域)导出的相同阈值用于研究中的其他位置(未吞噬的流域)区域。为了克服这种限制并考虑大区域内的阈值变异性,本文使用回归建模来预测通过将其与流域特性相关的阈值。这种方法对北卡罗来纳州的应用表明,阈值与主流坡,平均流域高度和平均流域坡面有关。通过使用FITNESS(F)和正确的(C)C> 0.9和F> 0.6的标准,结果显示了阈值预测和100年设计流的相应洪泛区与联邦应急管理局(FEMA)洪水的洪水相当该地区的保险利率地图(公司)。然而,拟议模型的洪泛平均值是低估的,并且在平均水平(平均流域坡度<1%)和山区(平均流域斜坡> 20%)中呈现过度估计。总的来说,拟议的方法提供了一种在数据稀缺区域中绘制洪泛区的替代方法。 (c)2017年Elsevier B.V.保留所有权利。

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