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Mass-balance changes of the debris-covered glaciers in the Langtang Himal, Nepal, from 1974 to 1999

机译:1974年至1999年尼泊尔朗塘喜玛拉尔邦覆盖的冰川的质量平衡变化

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摘要

Thick debris cover on glaciers can significantly reduce ice melt. However, several studies have suggested that debris-covered glaciers in the Himalaya might have lost mass at a rate similar to debris-free glaciers. We reconstruct elevation and mass changes for the debris-covered glaciers of the upper Langtang valley, Nepalese Himalaya, using a digital elevation model (DEM) from 1974 stereo Hexagon satellite data and the 2000 SRTM (Shuttle Radar Topography Mission) DEM. Uncertainties are high in the accumulation areas, due to data gaps in the SRTM and difficulties with delineation of the glacier borders. Even with these uncertainties, we obtain thinning rates comparable to those of several other studies in the Himalaya. In particular, we obtain a total mass balance for the investigated debris- covered glaciers of the basin of –0.320.18mw.e.a
机译:冰川上厚厚的碎屑覆盖物可以大大减少冰的融化。但是,一些研究表明,喜马拉雅山中覆盖有碎屑的冰川可能以与不含碎屑的冰川相似的速度损失了质量。我们使用1974年立体六边形卫星数据和2000 SRTM(穿梭雷达地形任务)DEM的数字高程模型(DEM),为尼泊尔喜马拉雅山Langtang谷地上覆盖有碎片的冰川重建了海拔和质量变化。由于SRTM中的数据空白以及冰川边界的描绘困难,在堆积区的不确定性很高。即使存在这些不确定性,我们也能获得与喜马拉雅山其他几项研究相当的细化率。特别是,我们对盆地进行了碎屑覆盖的冰川的总质量平衡为–0.320.18mw.e.a

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