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首页> 外文期刊>International journal of remote sensing >Monitoring glacier elevation and volume changes with digital photogrammetry and GIS at Gepatschferner glacier, Austria
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Monitoring glacier elevation and volume changes with digital photogrammetry and GIS at Gepatschferner glacier, Austria

机译:在奥地利Gepatschferner冰川使用数字摄影测量和GIS监测冰川海拔和体积变化

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摘要

Digital elevation models of Gepatschferner in Northern Tyrol, Austria were obtained with digital photogrammetry from high altitude stereo photo pairs and by digitizing an analogue topographic glacier map, for 1990 and 1971, respectively. A difference map was calculated to identify regions of glacier elevation increases and decreases corresponding to glacier mass gain and loss. While the glacier tongue below 2600 m showed mainly increases in glacier surface elevation as compared to 1971, the remaining glacier thickness experienced both increases and decreases. The accumulation zone above 3200 m contained several extreme cases of morphological features with altitude changes> + 30 m. While the increased ice thickness of the glacier tongue can be traced to a well documented period of mass accumulation in the 1970s, changes in glacier surface elevation in the higher zones may be linked either to the morphology of the glacier bed or to differences in insolation on the glacier surface. Between 1971 and 1990 the glacier experienced a net loss of 26 x 10~6m~3 corresponding to approximately 0.9% of the entire glacier volume.
机译:分别通过数字摄影测量法从高空立体照片对和数字化模拟地形冰川图(分别为1990年和1971年)获得了奥地利北蒂罗尔Gepatschferner的数字高程模型。计算差异图以识别对应于冰川质量增加和减少的冰川高程增加和减少区域。尽管与1971年相比,2600 m以下的冰川舌头主要表现出冰川表面高度的增加,但剩余的冰川厚度却经历了增加和减少。 3200 m以上的聚集带包含几种极端的形态特征,高度变化> + 30 m。虽然冰川舌头的冰厚增加可以追溯到1970年代有大量文献记载,但较高区域的冰川表面高程变化可能与冰川床的形态或日照的差异有关。冰川表面。 1971年至1990年之间,冰川净损失26 x 10〜6m〜3,约占整个冰川体积的0.9%。

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