首页> 外文会议>ACRS 2011;Asian conference on remote sensing >CLIMATE CHANGE AND LAND USE DYNAMICS; PERSPECTIVE ON SOIL EROSION AND SEDIMENTATION PROBLEM IN PHEWA LAKE WATERSHED AREA OF NEPAL
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CLIMATE CHANGE AND LAND USE DYNAMICS; PERSPECTIVE ON SOIL EROSION AND SEDIMENTATION PROBLEM IN PHEWA LAKE WATERSHED AREA OF NEPAL

机译:气候变化和土地利用动力学;尼泊尔费瓦湖流域地区的土壤侵蚀和沉积问题

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Phewa watershed area is in a fragile physiographic region, which intense monsoon rainfall one of highest rainfall receiving watershed of Nepal. The Phewa lake watershed covers the area of 118.19 km~2 and lies on Western Development Region of the country. The objective of this study is to find the land use dynamics and climate change effects on soil erosion and sedimentation problem in the watershed. The Phewa lake watershed is located in a steep slope terrain of the Himalaya mountain range as high. The precipitation plays the important role for the soil erosion and sedimentation. 30 years data of rainfall is analyze and see the scenario of change in climate of the watershed and the change in land use in watershed area. Phewa lake watershed area has significant marked of land use change and analyzed by using GIS technique. The land use change is due to the opening of the roads in the hilly areas connecting to the Pokhara valley. Most of the land use changes are found in all categories of the land cover. The effect of land use change directly shown to the soil erosion and sedimentation in the Phewa Lake. Direct observation survey also shows the tremendous effect in soil erosion and sedimentation. Barren land is completely disappearing changing to other land use. The rate of change of land use agriculture decrease (0.49% per annum), forest decrease (0.12% per annum) and built-up area increase (0.135%) per annum. Most of the changes are in settlement, agricultural land, and forest and build up area in the watershed. Adaptation and management of the settlement policy for the environmental perspective is the way of minimize the effects of climate change and land use dynamics with respect to soil erosion and sedimentation. Lake conservation can play the important role for minimizing the soil erosion and sedimentation problem in Phewa Lake. The study shows that the land use change is continuous process from one aspect to another aspect: man and nature are its major agents for change of the landscapes in the watershed area of the Phewa Lake.
机译:费瓦(Phewa)集水区位于脆弱的自然地理区,该地区强烈的季风降雨是尼泊尔接受降雨最多的流域之一。费瓦湖流域面积118.19 km〜2,位于该国西部开发区。这项研究的目的是发现土地利用动态和气候变化对流域水土流失和沉积问题的影响。 Phewa湖的分水岭位于喜马拉雅山脉的陡坡地带。降水在水土流失和沉积中起着重要作用。分析了30年的降雨数据,并观察了流域气候变化和流域地区土地利用变化的情景。费瓦湖流域具有明显的土地利用变化特征,并通过GIS技术进行了分析。土地用途的变化归因于连接博克拉山谷的丘陵地区道路的开通。在土地覆盖的所有类别中都可以找到大多数土地用途的变化。土地利用变化的影响直接反映在费瓦湖的土壤侵蚀和沉积中。直接观察调查还显示了对土壤侵蚀和沉积的巨大影响。贫瘠的土地正在完全消失,转而用于其他土地用途。土地利用农业的变化率每年减少0.49%,森林减少率每年0.12%,建成区增加率0.135%。大多数变化发生在定居点,农业用地,森林以及流域内的集聚区。从环境角度调整和管理移民政策是减少气候变化和土地利用动态对土壤侵蚀和沉积的影响的方法。湖泊保护对于减少费瓦湖的水土流失和沉积问题起着重要的作用。研究表明,土地利用变化从一个方面到另一个方面都是连续的过程:人与自然是改变Phewa湖流域区域景观的主要动因。

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