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Landform classification via fuzzy classification of morphometric parameters computed from digital elevation models: case study on Zagros Mountains

机译:通过数字高程模型计算的形态参数的模糊分类对地貌进行分类:以扎格罗斯山脉为例

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摘要

In this study, we investigate the use of morphometric parameters and fuzzy membership functions to perform landform classification for different case areas of Zagros Mountains from digital elevation models (DEMs). First, multiscale DEMs with scales of 5 to 45 cells are generated using the lifting scheme. The maximum curvature for the scale of five cells has the lowest standard deviation, and hence, is determined to be the characteristic scale. Data layers are produced from the DEM of this scale for slope, minimum and maximum curvatures, and plan and profile curvatures. The fuzzy membership rules for these data layers are used to determine the landform classes. Comparison of the results of landform classification using the fuzzy classification method and topographic position index (TPI) with the geology map of the study area show that the fuzzy classification method provides higher accuracy (81 %) as compared to TPI (42 %). This is because for the fuzzy classification method, sloping areas are separated into sloping and non-sloping areas, and the membership functions are defined to prevent landforms belonging to the sloping areas from being classified in the nonsloping areas and vice versa.
机译:在这项研究中,我们调查了使用形态计量学参数和模糊隶属函数从数字高程模型(DEM)对Zagros山的不同案例区域进行地貌分类的方法。首先,使用提升方案生成规模为5到45个单元的多尺度DEM。五个像元的刻度的最大曲率具有最低的标准偏差,因此被确定为特征刻度。从此比例的DEM生成数据层,以获取坡度,最小和最大曲率以及平面曲率和轮廓曲率。这些数据层的模糊隶属规则用于确定地形类别。使用模糊分类方法和地形位置指数(TPI)进行的地貌分类结果与研究区域的地质图的比较表明,与TPI(42%)相比,模糊分类方法提供了更高的准确性(81%)。这是因为对于模糊分类方法,将倾斜区域分为倾斜区域和非倾斜区域,并且定义了隶属函数以防止将属于倾斜区域的地貌分类到非倾斜区域中,反之亦然。

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