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Early 21st century spatially detailed elevation changes of Jammu and Kashmir glaciers (Karakoram-Himalaya)

机译:查和克什米尔冰川(Karakoram-Himalaya)在21世纪初的空间详细海拔变化

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Although a number of studies indicate the regional heterogeneity of the glacier elevation and mass changes in high-mountain Asia in the early 21st century, little is known about these changes with high spatial detail for some of the regions. In this study we present respective glacier elevation and mass change estimates in the Indian state of Jammu and Kashmir (JK) for the period 2000-2012. Our estimates are based on the interferometric analysis of SRTM DEM and the bistatic TanDEM-X data. On an average the JK East (Karakoram) glaciers showed less negative elevation changes (- 0.19 +/- 0.22myr(-1)) compared to the JK West (Himalaya) glaciers (-0.50 +/- 0.28 m yr(-1)). This agrees very well with previous studies that show a transition from larger changes in the western Himalaya to a steady-state situation in the Karakoram. We observe distinct elevation change patterns on a glacier scale that is most likely linked to debris insulation and the enhanced ice melting due to supraglacial lakes, ponds and ice cliffs. We also found 16 surge-type glaciers in the JK East which were not documented before. In total, 25 glaciers surged and 4 others appeared to be in a quiescent phase in the observation period. Our results also reveal that the glacier-averaged elevation change rates of surge-type and non surge-type glaciers in the JK East region are not significantly different.
机译:尽管许多研究表明,在21世纪初亚洲高山区亚洲冰川海拔和质量变化存在区域异质性,但对于某些区域的高空间细节这些变化知之甚少。在这项研究中,我们提出了2000-2012年印度查mu和克什米尔邦(JK)各自的冰川海拔高度和质量变化估计。我们的估算基于SRTM DEM的干涉测量分析和双基地TanDEM-X数据。与JK西(喜马拉雅山)冰川(-0.50 +/- 0.28 m yr(-1)相比,JK东(Karakoram)冰川平均显示出较少的负海拔变化(-0.19 +/- 0.22myr(-1))。 )。这与以前的研究非常吻合,以前的研究表明,喜马拉雅山西部地区发生了较大变化,而喀喇昆仑山脉则处于稳态。我们在冰川规模上观察到明显的海拔变化模式,这很可能与碎屑绝热以及冰川湖,池塘和冰崖引起的冰融化增强有关。我们还在JK East发现了16个浪涌型冰川,以前没有记录。在观测期间,总共有25座冰川涌动,另外4座冰川处于静止期。我们的研究结果还表明,JK East地区的浪涌型和非浪涌型冰川的冰川平均海拔变化率没有显着差异。

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