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An improved method of using icesat altimetry data to extract Tibetan Plateau glacier thickness change rate

机译:利用icesat测高数据提取青藏高原冰川厚度变化率的一种改进方法

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Glacier thickness change is a sensitive factor in response to global climate change, its quantitative assessment is critical to evaluate the variation of glacier mass balance. This paper analyzed and improved the method of planes fitted to repeat-tracks which uses Geoscience Laser Altimeter System (GLAS) data to extract glacier thickness change and applied it in the Tibetan Plateau area. The original plane fitting method was revised by curve fitting. Two extra parameters were added in the improved method so that the influence of complex terrain and of uncertainty due to sparse GLAS data on the estimate of glacier thickness change can be depressed. The improved method was applied to Naimona'Nyi glacier and Karakoram glacier in Tibetan Plateau area and results show that the glacier thinning rates reached -0.68±0.02 m/yr and -0.014±0.34m/yr respectively.
机译:冰川厚度变化是响应全球气候变化的敏感因素,其定量评估对于评估冰川质量平衡的变化至关重要。本文分析并改进了适用于重复轨道的平面方法,该方法利用地球科学激光测高仪系统(GLAS)数据提取冰川厚度变化并将其应用于青藏高原地区。最初的平面拟合方法通过曲线拟合进行了修改。在改进的方法中添加了两个额外的参数,以便可以抑制复杂地形和稀疏的GLAS数据导致的不确定性对冰川厚度变化估算的影响。将该方法应用于青藏高原奈莫纳尼冰川和喀喇昆仑山冰川,结果表明,冰川稀疏率分别达到-0.68±0.02 m / yr和-0.014±0.34m / yr。

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