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Application of remote sensing and GIS in sinuosity and river shifting analysis of the Ganges River in Uttarakhand plains

机译:遥感和GIS在北阿坎德邦平原恒河的曲率和河道分析中的应用

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Sinuosity and river shifting analysis of the Ganges River in Uttarakhand plains between Haridwar and Balawali has been done using topographic maps and various Landsat images during 1972 to 2005. The transect method was used for the river shiftingmeasurement. The study area consists of a stretch characterized by uneven meandering and shifting. Consequently, the adjacent areas are susceptible to frequent flooding that causes significant losses of crops, property, livestock, and human lives. During the study period, different channel patterns were observed such as straight singlechannel river, braided multi-channel river, etc. It was found that the west bank of the Ganges River was subjected to more erosion and that the river is shifting towards the west. The width of the meander belt ranged from 1 to 3.5 km with an average of about 2 km. Based on the findings of this study, it is suggested that the flood protection structures are crucial for the west bank. It is further suggested that these structures be constructed outside the meander belt of the river.
机译:利用地形图和各种Landsat影像,对1972年至2005年之间在哈里德瓦尔和巴拉瓦利之间的北阿坎德邦平原的恒河进行了正弦和河道分析。采用了横断面法进行河道测量。研究区域由伸展带组成,伸展带的曲折和移动不均匀。因此,邻近地区容易遭受频繁的洪水侵袭,从而造成庄稼,财产,牲畜和人类生命的重大损失。在研究期间,观察到了不同的河道模式,例如笔直的单河道河道,辫状的多河道河道等。研究发现,恒河西岸受到了更多的侵蚀,河道正在向西移动。曲折带的宽度范围为1至3.5 km,平均约2 km。根据这项研究的结果,建议防洪结构对于西岸至关重要。进一步建议将这些结构建在河的曲折带之外。

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