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首页> 外文期刊>Journal of Glaciology >Measuring daily surface elevation and velocity variations across a polythermal arctic glacier using ground-based photogrammetry
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Measuring daily surface elevation and velocity variations across a polythermal arctic glacier using ground-based photogrammetry

机译:使用基于地面的摄影测量法测量跨多极北极冰川的每日表面海拔和速度变化

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摘要

Twin time-lapse cameras were set up to provide a convergent view of ten targets located on the surface of an Arctic glacier, near its terminus. Using photogrammetric analysis, daily target elevations were calculated over three winters and two ablation seasons. Results show that the glacier surface level dropped by approximately 2.9 and 2.5 m respectively over the 2009 and 2010 ablation seasons. GPS measurements suggest the associated average vertical errors were 0.105 m and 0.04 m respectively. Photogrammetric measurements indicated that thinning from melting exceeded surface gains due to ice inflow by a factor of similar to 5:1 during 2009 and 2010. Horizontal flow rates of 6-12 mm d(-1) were measured photogrammetrically during autumn 2008 and compared to interpolated winter rates established from GPS measurements, with differences ranging between 7.4% and 17.2%. The availability of a continuous series of data for the duration of the study allowed the start and end dates of each ablation season to be identified, making it possible to determine the length of each balance year. The results show the utility of time-series photogrammetry for observing surface elevation changes and dynamic processes in remote glacial environments.
机译:设置了两个延时摄影机,以提供位于北极冰川终点附近的十个目标的汇聚视图。使用摄影测量分析,计算了三个冬季和两个消融季节的每日目标海拔高度。结果表明,在2009年和2010年消融季节,冰川表面水位分别下降了约2.9 m和2.5 m。 GPS测量表明,相关的平均垂直误差分别为0.105 m和0.04 m。摄影测量结果表明,融化的稀化超过了2009年和2010年由冰流入引起的表面增幅,约为5:1。2008年秋季,通过摄影测量法测量了6-12 mm d(-1)的水平流速,并将其与根据GPS测量结果得出的内插冬季率,差异在7.4%和17.2%之间。在研究期间可获得连续的一系列数据,可以确定每个消融季节的开始和结束日期,从而有可能确定每个平衡年的时长。结果表明,时间序列摄影测量法可用于观察偏远冰川环境中的表面高度变化和动态过程。

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