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首页> 外文期刊>Journal of the Indian Society of Remote Sensing >Extraction of Glacio-Geomorphological Units of Tons River Watershed Based on Remote Sensing Techniques
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Extraction of Glacio-Geomorphological Units of Tons River Watershed Based on Remote Sensing Techniques

机译:基于遥感技术的吨河流域冰川地貌单位提取

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Tons basin has the maximum share of glaciers, more than 50 glaciers, as well as glacierised area in Uttarakhand and Himachal Pradesh and the majority of the glaciers are of valley type. One of the important features of the glaciers of Tons valley is the presence of a thick mantle of supraglaciers moraine cover which can be attributed to the terrain characteristics, besides, the avalanche fed nature of the glaciers. The present study is the extraction of Glacio-geomorphological unit of Tons River basin based on the visual interpretation of remote sensing data. It was very much difficult in field, to extract all glacio-geomorphological units in glaciated area, but based on the remote sensing data, it becomes easy to identify. With the help of glacio-geomorphological map it has been found that four most important glaciers which fed the Tons River are Bandarpunch Glacier, Jaundar Bamak glacier, Jhajju Bamak and Tilku glacier. The tributaries of Tons River i.e. Harkidun Gad, Rupin Nadi and Supin Nadi are mainly fed by the mountain glaciers, valley glaciers and glacier lakes. The erosional terraces, glacio-fluvial terraces, open "U" shaped valleys, proglacial lake, lateral moraines, terminal moraines, palaeo-cirque and debris/talus cones are well developed in this glaciated regions. Glacio-geomorphic features are very much significant for palaeo-climatic reconstruction, showing variations, temporally and spatially. At the same time, these landforms, which are also altered by processes prevailing during interglacial period, helps in the geo-environment studies and glacier related problems like avalanches, global warming and cloudburst etc.
机译:吨山盆地的冰川所占比例最大,超过50个冰川,以及在北阿坎德邦和喜马al尔邦的冰川化地区,大多数冰川属于山谷型。吨山河谷的冰川的重要特征之一是存在上层冰m的厚覆盖层,这可归因于地形特征,此外还有冰川的雪崩补给性质。本研究是基于对遥感数据的可视化解释,提取Tons河流域的冰川-地貌单元。在野外提取冰川地区的所有冰川-地貌单位是非常困难的,但是基于遥感数据,它很容易识别。在冰川-地貌图的帮助下,发现了滋补吨斯河的四个最重要的冰川是班达蓬奇冰川,黄道·巴马克冰川,贾祖·巴马克冰川和提尔库冰川。吨斯河的支流,即Harkidun Gad,Rupin Nadi和Supin Nadi,主要由高山冰川,山谷冰川和冰川湖供食。在这个冰川地区,侵蚀性阶地,冰川-河流阶地,开阔的“ U”形山谷,冰川湖,侧向冰,、末端向冰,、古圆形和碎屑/距骨锥都非常发达。冰川地貌特征对于古气候重建非常重要,在时间和空间上都表现出变化。同时,这些地貌也因间冰期盛行的过程而改变,有助于进行地球环境研究以及与雪崩,全球变暖和暴云等冰川相关的问题。

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