INVESTIGATION OF CRYOSPHERE DYNAMICS VARIATIONS IN THE UPPER INDUS BASIN USING REMOTE SENSING AND GIS

J. Iqbal, M. Ali, Amjad Ali, D. Raza, F. Bashir, F. Ali, S. Hussain, Z. Afzal
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引用次数: 2

Abstract

Abstract. Glaciers are storehouses for freshwater. Glaciers Monitoring is one of the most important research areas especially when climate change has been accelerated snowmelt process. The major goal of research was to find snow cover trend for glaciated regions of Pakistan followed by estimation of snow mass balance. The area chosen for it was Upper Indus basin, which includes ranges of Hindukush, Karakoram and Himalayas extended in Pakistan, India and China. This region exhibits high topographic relief and climate change variability. Snow cover trend analysis was performed for eleven years ranging from 2004 to 2014 using Moderate Resolution Imaging Spectroradiometer (MODIS) data imagery product with daily temporal resolution. These results were combined with respective year’s average monthly temperature. Further quantitative analysis was performed to relate presence of greater vegetation as an indication of greater snowmelt using Landsat Imagery for these years. Snow mass balance curves reveal that glaciers are regaining their mass balance after losing mass balance in middle of last decade. In addition to that, only freely available data is used for this study. This purpose behind this approach is to prove RS and GIS has an effective and low-cost tool for snow cover monitoring, also mass balance calculations. Continuous monitoring of snow cover dynamics is effective for prediction and mitigation of hazards associated with areas in proximity of glaciated regions. One common hazard is glacial lake outburst phenomenon, which cause severe flash flooding in downstream areas. Year 2004 has the lowest mass snow balance and 2014 has the highest snow mass balance. These different parameters were analysed and results show that snow start melting in months of May and June and faster melting rate observed in months of July and August. With the advancement in computing technologies, it has been easier for computers to handle and manipulate massive datasets. Remote sensing has proved to be an excellent tool for extraction of data from glaciers, snow and oceans for remote areas. In particular, snow cover/snowmelt can tell us continuously changing melting patterns, which helps concerned authorities to take necessary measures for preserving these storehouses of water and to mitigate effect of global warming.
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基于遥感和gis的印度河上游流域冰冻圈动力学变化研究
摘要冰川是淡水的仓库。冰川监测是气候变化加速融雪过程的重要研究领域之一。研究的主要目标是发现巴基斯坦冰川地区的积雪趋势,然后估计雪质量平衡。选定的地区是上印度河盆地,包括印度库什山脉、喀喇昆仑山脉和喜马拉雅山脉,延伸到巴基斯坦、印度和中国。该地区地形起伏度高,气候变化多变性强。利用日时间分辨率的MODIS数据影像产品对2004 - 2014年11年的积雪趋势进行了分析。这些结果与相应年份的月平均温度相结合。使用陆地卫星图像进行了进一步的定量分析,将这些年来出现的更多植被作为更多融雪的指示。雪质量平衡曲线显示冰川在近十年中期失去质量平衡后,正在恢复其质量平衡。除此之外,本研究仅使用可免费获得的数据。这种方法背后的目的是证明RS和GIS是一种有效和低成本的积雪监测工具,也是一种质量平衡计算工具。持续监测积雪动态对于预测和减轻与冰川区域附近地区有关的危害是有效的。常见的灾害之一是冰湖溃决现象,造成下游地区严重的山洪暴发。2004年整体雪平衡最低,2014年整体雪平衡最高。对这些参数进行了分析,结果表明,5月和6月积雪开始融化,7月和8月融化速度更快。随着计算机技术的进步,计算机处理和操作海量数据集已经变得更加容易。事实证明,遥感是为偏远地区从冰川、积雪和海洋中提取数据的一种极好的工具。特别是,积雪/融雪可以告诉我们不断变化的融化模式,这有助于有关当局采取必要的措施来保护这些储水库,减轻全球变暖的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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