首页> 外文期刊>Journal of Hydrology >Glacier mass changes in Rongbuk catchment on Mt. Qomolangma from 1974 to 2006 based on topographic maps and ALOS PRISM data
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Glacier mass changes in Rongbuk catchment on Mt. Qomolangma from 1974 to 2006 based on topographic maps and ALOS PRISM data

机译:珠峰绒布流域的冰川质量变化。基于地形图和ALOS PRISM数据的1974至2006年珠穆朗玛峰

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Elevation changes of glacier surfaces were investigated in Rongbuk Catchment (RC) on the northern slopes of Mt. Qomolangma in the central Himalayas, by comparing a digital elevation model (DEM) generated from the 2006 ALOS/PRISM imageries with the base DEM1974 derived from the 1:50,000 topographic maps. The average elevation change rate of glacier surfaces in RC was estimated at -0.47 +/- 0.23 m a(-1) between 1974 and 2006. Such surface lowering rates varied significantly with glaciers and altitudes. One of the notable results is that the debris-covered ice thinned much more rapidly than the exposed ice at higher altitudes. Overall, glaciers in RC have lost mass of -0.06 +/- 0.04 Gt a(-1) during 1974-2006. Glacier imbalance constitutes about 50% or more of the Rongbuk runoff. (C) 2015 Elsevier B.V. All rights reserved.
机译:在山北坡的荣布集水区(RC)调查了冰川表面的高程变化。通过比较2006年ALOS / PRISM影像生成的数字高程模型(DEM)与1:50,000地形图得出的基础DEM1974,比较喜马拉雅中部的Qomolangma。在1974年至2006年之间,RC冰川表面的平均海拔变化率估计为-0.47 +/- 0.23 m a(-1)。此类表面下降率随冰川和海拔高度的变化而显着变化。值得注意的结果之一是,在更高的海拔高度,被残骸覆盖的冰的稀化速度比暴露的冰要快得多。总体而言,RC冰川在1974-2006年间的质量损失为-0.06 +/- 0.04 Gt a(-1)。冰川失衡构成了融北径流的约50%或更多。 (C)2015 Elsevier B.V.保留所有权利。

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