首页> 外文期刊>Journal of Glaciology >Elevation changes of glaciers revealed by multitemporal digital elevation models calibrated by GPS survey in the Khumbu region, Nepal Himalaya, 1992-2008
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Elevation changes of glaciers revealed by multitemporal digital elevation models calibrated by GPS survey in the Khumbu region, Nepal Himalaya, 1992-2008

机译:尼泊尔喜马拉雅山昆布地区通过GPS测量校准的多时相数字高程模型揭示的冰川高程变化

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摘要

Due to remoteness and high altitude, only a few ground-based glacier change studies are available in high-mountain areas in the Himalaya. However, digital elevation models based on remotely sensed data (RS-DEMs) provide feasible opportunities to evaluate how fast Himalayan glaciers are changing. Here we compute elevation changes in glacier surface (total area 183.3km2) in the Khumbu region, Nepal Himalaya, for the period 1992-2008 using multitemporal RS-DEMs and a map-derived DEM calibrated with differential GPS survey data in 2007. Elevation change is calculated by generating a weighted least-squares linear regression model. Our method enables us to provide the distribution of uncertainty of the elevation change. Debris-covered areas show large lowering rates. The spatial distribution of elevation change shows that the different wastage features of the debris-covered glaciers depend on their scale, slope and the existence of glacial lakes. The elevation changes of glaciers in the eastern Khumbu region are in line with previous studies. The regional average mass balance of -0.40±0.25mw.e. a ~(-1) for the period 1992-2008 is consistent with a global value of about -0.55mw.e. av ~(-1) for the period 1996-2005.
机译:由于地处偏远和海拔高,在喜马拉雅山的高山地区仅有少数基于地面的冰川变化研究。但是,基于遥感数据(RS-DEM)的数字高程模型提供了评估喜马拉雅冰川变化速度的可行机会。在这里,我们使用多时相RS-DEMs和基于地图的DEM(使用2007年差分GPS调查数据校准)计算了尼泊尔喜马拉雅山昆布地区冰川表面(总面积183.3km2)的海拔变化。通过生成加权最小二乘线性回归模型来计算。我们的方法使我们能够提供高程变化的不确定性分布。杂物覆盖的区域下降速度很大。高程变化的空间分布表明,残骸覆盖冰川的不同浪费特征取决于其规模,坡度和冰川湖泊的存在。昆布东部地区冰川的海拔变化与以前的研究一致。区域平均质量平衡为-0.40±0.25mw.e。 1992-2008年期间的〜(-1)与-0.55mw.e的全球价值一致。e。 1996年至2005年的平均(-1)。

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