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Areas of Glaciers and Glacial Lakes in North-Eastern Nepal studied with Landsat Imagery between 1992 and 2015

机译:在1992年至2015年之间,利用Landsat影像研究了尼泊尔东北部的冰川和冰川湖地区

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The passive remote sensing of Landsat images gives a great opportunity to look at the glaciers and the glacial lakes in the Himalayas and construct a time series to assess the changes which has occurred over the years. After analyzing different methods to map clean glaciers, debris covered glaciers and glacial lakes, a method combining supervised classification of the Landsat image and morphometric parameters (slope and aspect) derived from global digital elevation model (ASTER GDEM) was applied to map the glaciers and glacial lakes in the northeastern Himalayas of Nepal and bordering areas of Tibetan plateau. Furthermore, manual intervention was also done for the debris covered glaciers and glacial lakes to reduce the noises and improve the accuracy. A time series was constructed after mapping which included the years 1992,1995,1998,2008 and 2015 with 1992 as the reference year. An apparent melting trend for the clean glaciers was seen with coefficient of regression of 0.56 and a loss rate of-10.54 km2 per year for the period of 23 years (1992-2015). For the debris covered glaciers and glacial lakes, a fluctuating behavior with no trend was seen. However, a clear trend of expansion of the supraglacial lakes on top of the debris covered glaciers was seen with the regression coefficient of more than 0.9 and a rate of expansion of 0.11 km~2 per year. A total of 6 lakes in the study area were seen to be expanding significantly since 1992.Although glaciers and glacial lakes could be mapped with satisfactory results, the results could be improved by using high resolution imagery in combination with Landsat. Moreover, using radar based remote sensing to map the glaciers and glacial lakes in the Himalayas could mitigate the problem of cloud cover which was one of the major hindrances in this study.
机译:Landsat影像的被动遥感为观察喜马拉雅山的冰川和冰川湖提供了一个绝佳的机会,并建立了一个时间序列来评估多年来发生的变化。在分析了用于绘制清洁冰川,碎屑覆盖的冰川和冰川湖泊的各种方法之后,将Landsat图像的监督分类与从全球数字高程模型(ASTER GDEM)导出的形态参数(坡度和纵横比)相结合的方法应用于冰川尼泊尔东北喜马拉雅山和青藏高原接壤地区的冰川湖。此外,还对覆盖冰川和冰川湖的碎片进行了人工干预,以减少噪音并提高准确性。经过映射后构造了一个时间序列,其中包含1992、1995、1998、2008和2015年,其中以1992年为参考年。在23年期间(1992年至2015年),清洁冰川的融化趋势明显,回归系数为0.56,每年的损失率为-10.54 km2。对于碎片覆盖的冰川和冰川湖,没有波动的趋势。然而,在碎屑覆盖的冰川之上,冰川湖的扩张趋势明显,其回归系数大于0.9,每年的扩张速度为0.11 km〜2。自1992年以来,研究区域内共有6个湖泊正在显着扩展。尽管可以绘制冰川和冰川湖的图并获得令人满意的结果,但将高分辨率图像与Landsat结合使用可以改善结果。此外,使用基于雷达的遥感来绘制喜马拉雅山脉的冰川和冰川湖,可以减轻云层覆盖的问题,而云层覆盖是本研究的主要障碍之一。

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