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Climate Change and its Impact on Glaciers in Hindu Kush Region: A Case Study of Yarkhun Valley, Chitral Pakistan

机译:印度科苏河地区的气候变化及其对冰川的影响 - 以yh巴基斯坦玉蜀谷案例研究

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The impact of Climate change on water resources, especially glaciers, is an important issue today. Glaciers located in mountainous ranges namely the Alps, Himalaya, Karakoram and Hindu Kush have thousands of glaciers and glacial lakes. The Hindu Kush (HKH) glaciers, particularly the Chitral valley glaciers, are a visible indicator of climate change through the decrease of glacier cover area, recently formed glacial lakes and the increase of glacial lake outburst flood events. This paper presents a spatiotemporal analysis of precipitation and temperature trends and a GIS&RS base investigation of the related glacier dynamic in Yarkhun valley Chitral district. Temporal glacier coverage was delineated using objected base classification coupled with manual digitization of accurate glacier outline in the debris cover area with high resolution imagery. Finally, the results were validated with field data acquired from field assessment and ICIMOD inventory data. Trend and correlation analysis for the period of 1990 to 2010 at 2 climate stations and 10 weather monitoring posts (WMPs) shows that there is 1.2 degree increase in annual temperature and an increase of 20 mm for precipitation. Temporal dynamic analysis Yarkhun valley glaciers shows that there is a decrease of snow and glacier cover area -from 679.61 to 632.54 sq.km and an increase of debris cover area - from 60.52 to 84.51 sq.km between 2000 and 2015. Overall the glaciers of Yarkhun valley glacier faces are retreating and the need for vigilance in assessing glacier behaviors regarding climate change is apparent.
机译:气候变化对水资源,特别是冰川的影响是今天的一个重要问题。位于山区范围内的冰川即阿尔卑斯山,喜马拉雅,卡拉科拉姆和印度教犬有成千上万的冰川和冰川湖泊。印度犬(HKH)冰川,特别是十四谷山谷冰川,是通过冰川覆盖面积的减少,最近形成冰川湖泊和冰川湖爆发洪水事件的增加,是气候变化的可见指标。本文提出了对玉春谷区相关冰川动态的降水和温度趋势和GIS和RS基础调查的时尚分析。使用具有高分辨率图像的碎屑覆盖区域的精确冰川轮廓的手动数字化逐个绘制时间冰川覆盖范围。最后,通过从现场评估和ICIMOD库存数据获取的现场数据验证了结果。 1990年至2010年的趋势和相关分析在290年至2010年,在2个气候站和10个天气监测柱(WMPS)表明年度温度增加1.2度增加,降水量增加20毫米。时间动态分析Yarkhun Valley Glaciers表明,从679.61至632.54平方米和碎片覆盖区域增加到679.61至632.54平方米,从60.52到84.51平方米,2000年至2015年之间。总体而言Yarkhun Valley Glacier Faces正在撤退,并且在评估关于气候变化的冰川行为方面的警惕性是明显的。

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