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Recent retreat of the Elbrus glacier system

机译:布鲁斯冰川系统最近的退缩

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摘要

The glacier system covering Europe's highest mountain, Elbrus, has exhibited an accelerated retreat since 1980. Some studies have related this retreat to a significant summer temperature increasing trend. Relief- and aspect-related parameters for the glacierized area have an important impact on glacier changes. In this paper, the changes in glacier area are identified, quantified and correlated with relief parameters for the period 1985-2007. Spatial analysis was performed using the GLAM-CD (Glacier Mapper Change Detector) algorithm. The input data for this algorithm were Landsat 5 images, the Aster Global Digital Elevation and the glacier outlines from the GLIMS project (Global Land Ice Measurements from Space). Regression analyses between glacier area losses and relief-related parameters indicate a significant positive relation with the altitude and a significant negative relation with the glacier surface area. In this context, we used a correlated component regression to model these relations. The model explains >50% of the total variation.
机译:自1980年以来,覆盖欧洲最高峰Elbrus的冰川系统便出现了加速退缩。一些研究已将该退缩与夏季气温明显升高的趋势相关联。冰川化地区的与地形相关的参数对冰川变化具有重要影响。在本文中,对冰川面积的变化进行了识别,量化并与1985-2007年期间的起伏参数相关联。使用GLAM-CD(冰川映射器变化检测器)算法进行空间分析。该算法的输入数据是Landsat 5图像,Aster全球数字高程和GLIMS项目(来自太空的全球陆地冰测量)的冰川轮廓。冰川面积损失与浮雕相关参数之间的回归分析表明,与海拔高度呈显着正相关,与冰川表面积呈显着负相关。在这种情况下,我们使用相关分量回归对这些关系进行建模。该模型解释了总变化的> 50%。

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