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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高度数据提取藏高平台冰川厚度变化率的改进方法

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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:冰川厚度变化是对全球气候变化的敏感因素,其定量评估对于评估冰川大规模平衡的变化至关重要。本文分析并改进了安装在重复轨道的飞机方法,该方法使用地球科学激光高度计系统(GLAS)数据提取冰川厚度变化并将其应用于西藏高原地区。通过曲线配件修改原始平面拟合方法。在改进的方法中加入了两种额外参数,以便可以抑制复杂地形和由于稀疏GLAS数据引起的不确定性的影响。可以抑制冰川厚度变化的估计。将改进的方法应用于泰国高原地区的奈莫纳的冰川和喀喇昆仑冰川,结果表明,冰川稀释率分别达到-0.68±0.02 m / yr和-0.014±0.34米/毫升。

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