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GIS Based landform classification using digital elevation model: a case study from two river basins of Southern Western Ghats, Kerala, India

机译:基于GIS的地形分类使用数字高度模型 - 以南部南部山谷,印度喀拉拉邦两岸河流分类

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The main purpose of this study is to classify/characterize the landforms within a river basin using complex spatial information and GIS application to recognize and extort geomorphologic properties of Digital Elevation model with 30?m resolution. The landform classification is based on the Topographic position index (TPI) of the area under study—the Ithikkara and Kallada river basins, Southern Western Ghats, Kerala, India. The TPI generated was used for classifying the landscape to slope position index and landform classes. The slope position classes identified are Ridges/Hilltop/Canyon edge, Upper slope, Mid slope, Flat, Lower slope and Valley. The Landform classes includes (1) Canyons, deeply incised streams, (2) Midslope drainages, shallow valleys, (3) Upland drainages, headwaters, (4) U-shaped valleys, (5) Plains, (6) Open slopes, (7) Upper slopes, mesas, (8) Local ridges/hills in valleys, (9) Midslope ridges, small hills in plains and (10) Mountain tops, high ridges. 50.23% of the study area belongs to the slope position class—Ridges/Hilltop/Canyon edge. 30% of the study area is occupied by the landform class Canyons and deeply incised streams followed by Mountain tops and high ridges which covers 28.16%. The U shaped valleys represent 12.32% of the study area. The validation of landform classes is done by overlaying the stream network of the basin is into the landform classes, which is perfectly overlapping with the U shaped valleys of the landform classes. The classification of landform from the study can be used in applications related to precision agriculture, land use alteration studies where the most dominant factor is landform.
机译:本研究的主要目的是使用复杂的空间信息和GIS应用来分类/表征河流盆地内的地貌,以识别和敲入数字高度模型的整晶性质,分辨率为30?地形分类基于研究区域的地形位置指数(TPI) - Ithikkara和Kallada河流域,南部霍斯,喀拉拉邦,印度。生成的TPI用于将景观分类为斜坡位置指数和地形等级。识别的斜坡位置等级是脊/山顶/峡谷边缘,上坡,中坡,平,下坡和山谷。地形等级包括(1)峡谷,深度切开的流,(2)中间板排水,浅谷,(3)高地排水,返波,(4)U形谷,(5)平原,(6)开口斜坡,( 7)上斜坡,梅萨斯,(8)山谷的当地山脊/山丘,(9)中间板脊,平原的小山丘和(10)山顶,高脊。 50.23%的研究区域属于斜坡位置脊/山顶/峡谷边缘。 30%的研究区由地形级峡谷占用,深入切割的山顶,其次是山顶和高脊,占地28.16%。 U形山谷占研究区的12.32%。地形等级的验证是通过覆盖盆地的流网络进入地形等级的验证,这与地形等级的U形谷完全重叠。该研究的地貌分类可用于与精密农业有关的应用,土地利用改变研究,其中最主要的因素是地貌。

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